Tien Shan
Summary
- Network Code: XW
- Experiment duration: 1999-04 to 2001-12
- Number of events: 22184
- Prinicpal investigators: Frank Vernon
- Download dataless SEED volume
Introduction
What is the Tien Shan Network?
The Tien Shan network is composed of the KNET, Kaznet and GHENGIS digital broadband stations and together they contribute to the Central Asia Bulletin.
The Tien Shan network records earthquakes both locally as well as globally. These data are useful in a number of geophysical problems. For example, local recordings of teleseisms can be used in teleseismic tomography studies and to address seismotectonic problems.
Summary of activities
- Deployed 28 PASSCAL mode portable temporary stations in the Tien Shan region that recorded data from over the course of two years.
- Recorded, located and archived data (e.g., waveforms, locations) from ~13,800 earthquakes.
- Routinely provided our data sets in a timely manner to the IRIS Data Management Center.
- Enhanced computer software:
- Cubic-spline interpolation routines to resample data at a higher sample rate.
- Removed obsolete coding from the Got et al., 1994 waveform cross-correlation programs.
- Began updating the computer codes of Got et al., 1994 to use Antelope formatted data.
- We presented a paper titled "A Central Asian Seismic Bulletin: Utilizing the KNET, Kaznet, and Tien Shan Data Sets" at the AGU meeting in December 2001.
- Based on work done during this funding period we presented a paper titled Gauging (in)accuracy of mainshock focal mechanisms from (anti)correlations of aftershock locations and regions of positive static Coulomb stress changes at the IRIS meeting in June 2002.
- Based on work done during this funding period we are preparing a paper titled Aftershock Focal mechanism Heterogeneity: Why & Where for publication in BSSA.
Major findings over the project duration
- We deployed and operated a seismic network in Tien Shan (Figure 1a & 1b).
- For local earthquakes, the magnitude of completeness for the Tien Shan catalog is magnitude ~2.5, which greatly exceeds the magnitude ~3.5 completeness levels of the other global catalogs (Figures 2a, 2b, 2c & 3 ).
- Compared earthquake locations (latitude, longitude, and depth) listed in the Tien Shan catalog with those listed in the PDE catalog ( Figure 4 ). For a representative data subset, the median difference between for latitude, longitude and depth are 0.45, 0.3 and 30 km, respectively.
- A cross section of local earthquakes in the Tien Shan region show shallow earthquakes in the north and deeper earthquakes in the south (near Hindu Kush - Figure 5 ).
- In the Xinjiang province of China, which is just south of the Tien Shan network, we find evidence of spatial seismic migration from the North-west to the South-east (Figures 6a & 6b ).
- For local Tien Shan earthquakes, we determine optimal parameters for waveform cross-correlation analyses (Figures 7 & 8 ): (1) optimal window length is 10 seconds; (2) optimal frequency band to perform cross-correlation analysis is 1-8 Hz; and (3) waveform correlation should only be preformed on sub-groups of earthquakes that extend over no more than a 5 km diameter region (any distances further than this violates the base assumptions in the correlation analyses).
- Tested each seismic stations data for suitability in waveform cross-correlation analyses. Obviously broadband stations with a high sample rate are preferred, but we find that after interpolation stations with a sample rate of only 20sps can also be beneficial to correlation studies.
- We investigate the assumption that most aftershocks rupture similarly oriented fault planes by cross-correlating and stacking data from two different aftershock sequences ( Figure 8 ). We find that, in general, ~75% of aftershocks rupture similarly oriented fault planes.
- We use Static Coulomb stress analysis and the distribution of aftershocks to gauge the viability of the mainshock focal mechanisms reported in the Harvard CMT catalog. We find evidence that the August 2nd, 1998 M6.1 mainshock focal mechanism may be in error (Figures 9 & 10 ).
Third year (2001-01-01 to 2001-12-31)
Comparison of earthquake locations from different network bulletins
In general, for local earthquakes, the Tien Shan catalog contains an order of magnitude more events than the global network catalogs, and the magnitude of completeness of the Tien Shan catalog is ~2.5, which greatly exceeds the completeness level of 3.5 of the global catalogs for local earthquakes in this region.
We compare the location (latitude, longitude and depth) of earthquakes determined from the Tien Shan network with data from global (e.g., PDE, REB & QED) and local (e.g., KIS) networks. We can only compare the larger magnitude events (M>3.5) because the global catalogs lack earthquakes of lower magnitude. The difference in latitude and longitude range between 0.2-0.8 and the median difference in depth ranges is 30km. The difference in depth is highly dependent on the 33 km depth that the PDE catalog assigns when the depth of an earthquake is unknown.
Assessing the depth range of the brittle faulting throughout the region
From ~93,000 earthquakes recorded by the Tien Shan network we see that the seismicity in Northern region of Tien Shan is shallower than that in the Southern regions. Although this depth variation is hinted at in other catalogs, the Tien Shan catalog shows this transition in more detail.
Recognition of seismicity migration
Seismicity patterns found in the Tien Shan catalog, in regions even on the edge of our network, are substantially more detailed than in other catalogs. For example, in the Xinjiang province of China, ~2000 earthquakes were recorded by the Tien Shan network during 1997-1999 that exhibit a clear spatial progression of seismicity. This progression, which is confined to a 50 km diameter region, is undetectable in other data catalogs, both global (e.g., REB, PDE, CMT) and local (KIS). The two largest earthquakes in this sequence were the M6.1 August 2, 1998, and the M6.2 August 27, 1998, earthquakes.
Seismic waveform Cross-correlation techniques
A problem-free seismic network with excellent azimutal coverage of the seismic area of interest and an acceptable model of the velocity structure does not guarantee precise earthquake locations can be determined. This is because location errors can result not only from uncertainties in the velocity model but also from uncertainties in the time of the seismic wave's arrival or misidentification of the seismic phases. New algorithms, based on seismic waveform cross-correlation, can account for uncertainties in arrival times and in some cases correct for misidentified phases. These methods make use of the fact that earthquakes from the same region (< 3 km) whose seismic waves travel the same path from source-to-station have similar waveforms. By correlating these similar waveforms sub-sample accuracy of seismic wave arrival times can often be attained. This, in turn, can reduce the relative errors in earthquake locations to tens or hundreds of meters, values that are often an order of magnitude smaller than the errors in the original catalogs.
We demonstrate the power of relocation methods that are based on waveform cross-correlations, with a simple example. Here, we begin by segmenting the data into 10 second windows which include the P-wave arrival time. We align all of the segmented data on the P-wave arrival time and produce a color-coded map of the waveform amplitudes and the resulting waveform stack. The jitter in the waveform stack, and randomness of the color-map, indicates the waveforms are not optimally aligned. We next repeat the process after correlating all waveforms with a master event. The waveform alignments have been greatly improved as indicated in the fringe pattern in the color map and reduction of noise in the stack. Further refinement is obtained by restricting the data to only event pairs that have a high correlation coefficients (>0.6).
For each station in the Tien Shan network, using all available data, we produced figures similar to Figure 7 to determine if the seismic waveforms are similar enough for cross-correlation analyses to be successful. We also test different frequency band filters with the aim to identify one that will eliminate most of the noise while not destroying important aspects of the signal. We find a bandpass filter of 1-8 Hz is optimal. Of the ~15 stations investigated, all are suitable for use in waveform cross-correlation studies.
The optimal alignment of two waveforms is not always indicated by the maximum correlation coefficient that results from a moving window comparison of the data pair. This problem is often due to cycle skips that occur when the seismic waveforms of interest have approximately constant amplitude for multiple cycles and are dominated by a single frequency. For a pair of seismic waveforms with these characteristics, results from a moving window cross-correlation test will have, at each cycle, a peak in the correlation coefficients. These multiple peaks will have approximately the same amplitude, and the maximum peak will not necessarily correspond to the best alignment. One way to avoid cycle skips is to correlate only very short segments of the waveforms. However, if the true P-wave arrival is not in the windowed segment again the method will still fail. This can happen if the automated P-wave arrival time is in error by more than the duration of a few cycles. The most robust way to avoid the cycle-skip problem is to assure the P-wave arrival is in the window of interest by using data that was processed by a seismic analyst. Because each earthquake (~13,800) in the Tien Shan catalog has been analyst reviewed, this data set is ideal for relocation analyses.
Even with the best data, waveform correlation techniques fail when there truly is minimal similarly in the waveforms. Reason for the minimal similarity include rupture on faults with distinctly different orientations, differences in the earthquake source processes (e.g., directivity variations) or near source velocity field variations. These properties may be controlled by the tectonic setting, the mainshock fault orientation and direction of fault slip, the orientation of pre-existing faults in the region, or the magnitude of the background stress field. A byproduct of our work that examines earthquakes with similar waveforms is the identification of those events with dissimilar waveforms. These data will be the focus of a future study.
Aftershock focal mechanism heterogeneity
Aftershock sequences are prime candidates for relocation analysis because of the large number of earthquakes that occur close together in both space and time. We examine the heterogeneity of two aftershock sequences in the Tien Shan region: the 2 August 1998 M6.1 earthquake and the 27 August 1998 M6.2 earthquake. One aim of this study is to determine if it is reasonable to assume a single aftershock fault orientation and slip direction for all aftershocks; an assumption that is often made to simplify computer calculations. We align and stack seismic waveforms based on the analyst picked P-wave arrivals. For better alignment we cross-correlate the waveforms with a master event. Before cross-correlation the fringe pattern, which represents similar seismic waveforms, is undetectable, but after cross-correlation sharpness of the stacks indicates that many of the waveforms are similar.
Correlation of Static Coulomb failure stress change and the spatial distribution of aftershocks
The spatial distribution of aftershocks can sometimes be used to estimate mainshock focal mechanisms. Aftershocks that distribute in a single widely- distributed cloud about the mainshock fault are often an indication of a primarily dipping fault in the region. Aftershocks that locate primarily in the hanging wall are often an indication that the mainshock was a thrust event instead of a normal event. Whereas, aftershocks that primarily distribute beyond the tip zones of the mainshock fault and distribute in two-to-four tear-drop cells are often an indication that the mainshock was a strike-slip event that ruptured a vertical faults. These teardrop shaped distributions typically span the entire depth of the mainshock fault plane. The spatial distributions of aftershocks we describe here can be predicted with theoretical models of static Coulomb failure stress change (CFS).
Static Coulomb failure stress change (CFS) analysis is routinely used to determine if one earthquake triggered another. A correlation between regions of mainshock induced stress increases and aftershock locations is often interpreted as evidence that the CFS model is viable; yet, uncertainties as small as ±30° in the mainshock/aftershock parameters (strike, dip, or rake) can introduce different outcomes. Thus, the most significant result is when a correlation is not attainable.
Maps of CFS are dependant on both the mainshock fault orientation and the aftershock fault orientation.
We applied Coulomb stress analysis to the two ~M6 earthquakes in the Xinjiang province of China. According to the Harvard moment tensor solutions, both events ruptured faults that trend parallel to the geologic structures in the region (~N55W). However, the August 27 event was a vertical strike slip event while the August 2 event ruptured a dipping fault and had a normal component of slip. These slip directions are counter to what we expect for this fold-and-thrust-belt that typically has earthquakes with thrust mechanisms.
We compute CFS models for a number of viable mainshock models of the August 2 event and find that there is minimal correlation between regions of DCFS increase and the aftershock locations. Instead, if we assume the mainshock earthquake was a thrust event, rather than a normal event, we find a strong correlation between regions of CFS increases and the aftershock locations. One explanation for the anti-correlation when normal slip is assumed is that uncertainties in the mainshock and aftershock fault planes are so large that accurate estimates of CFS are unattainable.
Second and first years
Data processing and data delivery to the IRIS Data Management Center.
Station List
sta ondate offdate lat lon elev staname statype refsta dnorth deast AAK 1992240 1993239 42.6333 74.4944 1.68 - ss - 0 0 AAK 1993305 1994241 42.6333 74.4944 1.68 - ss - 0 0 AAK 1996092 -1 42.6333 74.4944 1.68 - ss - 0 0 AAK 1991244 1992239 42.6333 74.4944 1.68 - ss - 0 0 AAK 1993240 1993304 42.6333 74.4944 1.68 - ss - 0 0 AAK 1994242 1996091 42.6333 74.4944 1.68 - ss - 0 0 AHQI 1999163 2001365 40.9347 78.4578 1.959 - ss - 0 0 AKSU 1999163 2001365 41.1441 80.1098 1.109 - ss - 0 0 AKT 1994274 -1 50.4348 58.0167 0.36 Aktyubinsk, Kazakstan ss - 0 0 AKTK 1999267 -1 50.4348 58.0167 0.36 Aktyubinsk, Kazakstan ss - 0 0 AML 1993305 1994241 42.1311 73.6941 3.4 - ss - -55.434 -65.88 AML 1994242 1996091 42.1311 73.6941 3.4 - ss - -55.434 -65.88 AML 1996092 -1 42.1311 73.6941 3.4 - ss - -55.434 -65.88 AML 1991244 1992239 42.1311 73.6941 3.4 - ss - -55.434 -65.88 AML 1993240 1993304 42.1311 73.6941 3.4 - ss - -55.434 -65.88 AML 1992240 1993239 42.1311 73.6941 3.4 - ss - -55.434 -65.88 ANA 1997271 2001365 42.7844 77.657 1.813 - ss - 0 0 ARA 1999174 2001365 41.8491 74.3292 1.484 - ss - 0 0 ATUS 1997271 2001365 39.716 76.1572 1.225 - ss - 0 0 BAY 1997190 -1 50.8264 75.5537 0.442 Bayanaul, Kazakstan ss - 0 0 BCHU 1997271 2001365 39.7933 78.7825 1.14 - ss - 0 0 BGK2 1992240 1993239 42.6451 74.2274 1.64 - ss - 1.344 -21.8 BGK2 1991244 1992239 42.6451 74.2274 1.64 - ss - 1.344 -21.8 BGK2 1993240 1993253 42.6451 74.2274 1.64 - ss - 1.344 -21.8 BRVK 1994244 -1 53.0581 70.2828 0.33 Borovoye, Kazakhstan - - 0 0 CHAT 1999195 2001365 40.918 76.5209 3.031 - ss - 0 0 CHK 1994204 -1 53.6762 70.6152 0.24 Chkalovo, Kazakstan ss - 0 0 CHKZ 1996015 -1 53.6762 70.6152 0.12 Chkalovo, Kazakstan ss - 0 0 CHM 1993240 1993304 42.9986 74.7513 0.655 - ss - 40.58 20.856 CHM 1993305 1994241 42.9986 74.7513 0.655 - ss - 40.58 20.856 CHM 1994242 1996091 42.9986 74.7513 0.655 - ss - 40.58 20.856 CHM 1991244 1992239 42.9986 74.7513 0.655 - ss - 40.58 20.856 CHM 1992240 1993239 42.9986 74.7513 0.655 - ss - 40.58 20.856 CHM 1996092 -1 42.9986 74.7513 0.655 - ss - 40.58 20.856 DGE 1998249 2001365 40.9869 74.469 2.941 - ss - 0 0 EKS2 1993305 1994241 42.6615 73.7772 1.36 - ss - 3.378 -58.542 EKS2 1991244 1992239 42.6615 73.7772 1.36 - ss - 3.378 -58.542 EKS2 1993240 1993304 42.6615 73.7772 1.36 - ss - 3.378 -58.542 EKS2 1994242 1996091 42.6615 73.7772 1.36 - ss - 3.378 -58.542 EKS2 1996092 -1 42.6615 73.7772 1.36 - ss - 3.378 -58.542 EKS2 1992240 1993239 42.6615 73.7772 1.36 - ss - 3.378 -58.542 ERPT 1999220 2000165 42.6011 76.0735 3.79 - ss - 0 0 HARA 1999174 2001365 40.1742 76.8367 1.585 - ss - 0 0 HLQI 1999163 2001365 40.8415 77.9643 2.241 - ss - 0 0 KAI 1998249 2001365 41.5681 75.0134 2.016 - ss - 0 0 KAR 1997271 2001365 42.4734 78.4003 1.778 - ss - 0 0 KARL 1999218 2001365 41.4733 77.3093 3.021 - ss - 0 0 KASH 1997271 2001365 39.5165 75.9243 1.31 - ss - 0 0 KAZ 1997271 2001365 41.3849 73.9437 1.404 - ss - 0 0 KBK 1992240 1993239 42.6564 74.9478 1.76 - ss - 2.663 37.012 KBK 1996092 -1 42.6564 74.9478 1.76 - ss - 2.663 37.012 KBK 1991244 1992239 42.6564 74.9478 1.76 - ss - 2.663 37.012 KBK 1994242 1996091 42.6564 74.9478 1.76 - ss - 2.663 37.012 KBK 1993305 1994073 42.6564 74.9478 1.76 - ss - 2.663 37.012 KBK 1993240 1993304 42.6564 74.9478 1.76 - ss - 2.663 37.012 KDJ 1997271 2001365 42.1326 77.1856 1.783 - ss - 0 0 KENS 1999218 2001365 42.3201 79.2362 2.805 - ss - 0 0 KHA 1997271 2001365 44.2081 73.9973 1.014 - ss - 0 0 KKL 1997190 -1 49.3387 75.3823 0.925 Karkalarinsk, Kazakstan ss - 0 0 KOPG 1999163 2001365 40.504 79.036 1.114 - ss - 0 0 KSA 1997271 2001365 41.5425 77.9257 3.398 - ss - 0 0 KUR 1994206 -1 50.7149 78.6208 0.24 Kurchatov, Kazakstan ss - 0 0 KURK 1996330 -1 50.7149 78.6208 0.24 Kurchatov, Kazakstan ss - 0 0 KZA 1996092 -1 42.0778 75.2496 3.52 - ss - -61.384 62.22 KZA 1994242 1996091 42.0778 75.2496 3.52 - ss - -61.384 62.22 KZA 1993240 1993263 42.0778 75.2496 3.52 - ss - -61.384 62.22 KZA 1991244 1992239 42.0778 75.2496 3.52 - ss - -61.384 62.22 KZA 1992240 1993239 42.0778 75.2496 3.52 - ss - -61.384 62.22 MAK 1994207 -1 46.8075 81.9774 0.6 Makanchi, Kazakstan - - 0 0 MAKZ 1996258 -1 46.808 81.977 0.6 Makanchi, Kazakstan - - 0 0 NRN 1997271 2001365 41.423 75.9792 2.019 - ss - 0 0 PDG 1997271 2001365 43.3275 79.4876 1.286 - ss - 0 0 PIQG 1999171 2001365 40.3204 77.627 1.736 - ss - 0 0 POGR 1999195 2001365 41.0183 75.5502 2.357 - ss - 0 0 TERE 1999195 2001365 40.4757 75.7718 3.684 - ss - 0 0 TGMT 1999170 2001365 39.9956 76.139 1.823 - ss - 0 0 TKM 1993305 1994241 42.8601 75.3184 0.96 - ss - 25.502 67.044 TKM 1993240 1993304 42.8601 75.3184 0.96 - ss - 25.502 67.044 TKM 1991244 1992239 42.8601 75.3184 0.96 - ss - 25.502 67.044 TKM 1992240 1993239 42.8601 75.3184 0.96 - ss - 25.502 67.044 TKM2 1994257 1996091 42.9208 75.5966 2.02 - ss - 32.497 89.59 TKM2 1996092 -1 42.9208 75.5966 2.02 - ss - 32.497 89.59 TLG 1994208 -1 43.233 77.225 1.12 Talgar, Kazakstan - - 0 0 UCH 1993240 1993304 42.2275 74.5134 3.85 - ss - -45.044 1.562 UCH 1996092 -1 42.2275 74.5134 3.85 - ss - -45.044 1.562 UCH 1993305 1994241 42.2275 74.5134 3.85 - ss - -45.044 1.562 UCH 1994242 1996091 42.2275 74.5134 3.85 - ss - -45.044 1.562 UCH 1992240 1993239 42.2275 74.5134 3.85 - ss - -45.044 1.562 UCH 1991244 1992239 42.2275 74.5134 3.85 - ss - -45.044 1.562 ULHL 1996092 -1 42.2456 76.2417 2.04 - ss - -41.556 143.567 ULHL 1994252 1996091 42.2456 76.2417 2.04 - ss - -41.556 143.567 USP 1992240 1993239 43.2669 74.4997 0.74 - ss - 70.33 0.428 USP 1991244 1992239 43.2669 74.4997 0.74 - ss - 70.33 0.428 USP 1996092 -1 43.2669 74.4997 0.74 - ss - 70.33 0.428 USP 1993305 1994241 43.2669 74.4997 0.74 - ss - 70.33 0.428 USP 1993240 1993304 43.2669 74.4997 0.74 - ss - 70.33 0.428 USP 1994242 1996091 43.2669 74.4997 0.74 - ss - 70.33 0.428 VOS 1994205 -1 52.7232 70.9797 0.45 Vostochnoye, Kazakstan ss - 0 0 WQIA 1997271 2001365 39.7267 75.2473 2.17 - ss - 0 0 WUS 1988305 -1 41.199 79.218 1.457 Wushi, Xinjiang Uygur, China - - 0 0 XIKR 1999163 2001365 39.8178 77.3666 1.134 - ss - 0 0 ZRN 1994203 -1 52.951 69.0043 0.42 Zerenda, Kazakstan ss - 0 0 ZRNK 1995143 -1 52.951 69.0043 0.38 Zerenda, Kazakstan ss - 0 0
Total: 103
Channel List
sta chan ondate chanid offdate ctype edepth hang vang descrip AAK BHE 1996092 705 -1 n -0 90 90 - AAK BHE 1991244 444 1992239 n -0 90 90 - AAK BHE 1993240 564 1993304 n -0 90 90 - AAK BHE 1993305 612 1994241 n -0 90 90 - AAK BHE 1992240 477 1992261 n -0 90 90 - AAK BHE 1994242 660 1996091 n -0 90 90 - AAK BHN 1993240 563 1993304 n -0 0 90 - AAK BHN 1993305 611 1994241 n -0 0 90 - AAK BHN 1994242 659 1996091 n -0 0 90 - AAK BHN 1991244 443 1992239 n -0 0 90 - AAK BHN 1996092 704 -1 n -0 0 90 - AAK BHN 1992240 476 1992261 n -0 0 90 - AAK BHZ 1994242 658 1996091 n -0 0 0 - AAK BHZ 1996092 703 -1 n -0 0 0 - AAK BHZ 1992240 475 1992261 n -0 0 0 - AAK BHZ 1991244 442 1992239 n -0 0 0 - AAK BHZ 1993305 610 1994241 n -0 0 0 - AAK BHZ 1993240 562 1993304 n -0 0 0 - AAK BLE 1994242 663 1995005 n -0 90 90 - AAK BLE 1993240 567 1993304 n -0 90 90 - AAK BLE 1992261 507 1993239 n -0 90 90 - AAK BLE 1993305 615 1994241 n -0 90 90 - AAK BLN 1993240 566 1993304 n -0 0 90 - AAK BLN 1992261 506 1993239 n -0 0 90 - AAK BLN 1993305 614 1994241 n -0 0 90 - AAK BLN 1994242 662 1995005 n -0 0 90 - AAK BLZ 1992261 505 1993239 n -0 0 0 - AAK BLZ 1993240 565 1993304 n -0 0 0 - AAK BLZ 1994242 661 1995005 n -0 0 0 - AAK BLZ 1993305 613 1994241 n -0 0 0 - AAK HHE 1996092 414 -1 n -0 90 90 - AAK HHE 1992240 216 1993239 n -0 90 90 - AAK HHE 1994242 369 1996091 n -0 90 90 - AAK HHE 1993240 273 1993304 n -0 90 90 - AAK HHE 1991244 147 1992239 n -0 90 90 - AAK HHE 1993305 321 1994241 n -0 90 90 - AAK HHN 1991244 146 1992239 n -0 0 90 - AAK HHN 1994242 368 1996091 n -0 0 90 - AAK HHN 1993305 320 1994241 n -0 0 90 - AAK HHN 1993240 272 1993304 n -0 0 90 - AAK HHN 1996092 413 -1 n -0 0 90 - AAK HHN 1992240 215 1993239 n -0 0 90 - AAK HHZ 1993305 319 1994241 n -0 0 0 - AAK HHZ 1993240 271 1993304 n -0 0 0 - AAK HHZ 1996092 412 -1 n -0 0 0 - AAK HHZ 1991244 145 1992239 n -0 0 0 - AAK HHZ 1992240 214 1993239 n -0 0 0 - AAK HHZ 1994242 367 1996091 n -0 0 0 - AAK HLE 1993240 276 1993304 n -0 90 90 - AAK HLE 1992240 213 1993239 n -0 90 90 - AAK HLE 1991244 150 1992239 n -0 90 90 - AAK HLE 1993305 324 1994241 n -0 90 90 - AAK HLE 1994242 372 1995006 n -0 90 90 - AAK HLN 1993240 275 1993304 n -0 0 90 - AAK HLN 1992240 212 1993239 n -0 0 90 - AAK HLN 1994242 371 1995006 n -0 0 90 - AAK HLN 1991244 149 1992239 n -0 0 90 - AAK HLN 1993305 323 1994241 n -0 0 90 - AAK HLZ 1992240 211 1993239 n -0 0 0 - AAK HLZ 1991244 148 1992239 n -0 0 0 - AAK HLZ 1993240 274 1993304 n -0 0 0 - AAK HLZ 1994242 370 1995006 n -0 0 0 - AAK HLZ 1993305 322 1994241 n -0 0 0 - AAK LHE 1998160 738 -1 n -0 90 90 - AAK LHN 1998160 737 -1 n -0 0 90 - AAK LHZ 1998160 736 -1 n -0 0 0 - AHQI BHE 1999163 51 2001365 n -0 90 90 - AHQI BHN 1999163 50 2001365 n -0 0 90 - AHQI BHZ 1999163 49 2001365 n -0 0 0 - AKSU BHE 1999163 48 2001365 n -0 90 90 - AKSU BHN 1999163 47 2001365 n -0 0 90 - AKSU BHZ 1999163 46 2001365 n -0 0 0 - AKT BHE 1994274 742 -1 n 0 90 90 - AKT BHN 1994274 743 -1 n 0 0 90 - AKT BHZ 1994274 744 -1 n 0 0 0 - AKT HHE 1994274 775 -1 n 0 90 90 - AKT HHN 1994274 776 -1 n 0 0 90 - AKT HHZ 1994274 777 -1 n 0 0 0 - AKTK BHE 1999267 787 -1 n 0 90 90 - AKTK BHN 1999267 788 -1 n 0 0 90 - AKTK BHZ 1999267 789 -1 n 0 0 0 - AKTK HHE 1999267 790 1999268 n 0 90 90 - AKTK HHE 1999268 808 -1 n 0 90 90 - AKTK HHN 1999267 791 1999268 n 0 0 90 - AKTK HHN 1999268 809 -1 n 0 0 90 - AKTK HHZ 1999267 792 1999268 n 0 0 0 - AKTK HHZ 1999268 810 -1 n 0 0 0 - AML BHE 1993305 594 1994241 n -0 90 90 - AML BHE 1993240 540 1993304 n -0 90 90 - AML BHE 1992240 465 1992261 n -0 90 90 - AML BHE 1991244 432 1992239 n -0 90 90 - AML BHE 1996092 693 -1 n -0 90 90 - AML BHE 1994242 642 1996091 n -0 90 90 - AML BHN 1992240 464 1992261 n -0 0 90 - AML BHN 1993240 539 1993304 n -0 0 90 - AML BHN 1993305 593 1994241 n -0 0 90 - AML BHN 1994242 641 1996091 n -0 0 90 - AML BHN 1996092 692 -1 n -0 0 90 - AML BHN 1991244 431 1992239 n -0 0 90 - AML BHZ 1993305 592 1994241 n -0 0 0 - AML BHZ 1991244 430 1992239 n -0 0 0 - AML BHZ 1994242 640 1996091 n -0 0 0 - AML BHZ 1992240 463 1992261 n -0 0 0 - AML BHZ 1996092 691 -1 n -0 0 0 - AML BHZ 1993240 538 1993304 n -0 0 0 - AML BLE 1994242 645 1995005 n -0 90 90 - AML BLE 1992261 495 1993239 n -0 90 90 - AML BLE 1993305 597 1994241 n -0 90 90 - AML BLE 1993240 543 1993304 n -0 90 90 - AML BLN 1992261 494 1993239 n -0 0 90 - AML BLN 1994242 644 1995005 n -0 0 90 - AML BLN 1993305 596 1994241 n -0 0 90 - AML BLN 1993240 542 1993304 n -0 0 90 - AML BLZ 1994242 643 1995005 n -0 0 0 - AML BLZ 1993240 541 1993304 n -0 0 0 - AML BLZ 1993305 595 1994241 n -0 0 0 - AML BLZ 1992261 493 1993239 n -0 0 0 - AML HHE 1994242 351 1996091 n -0 90 90 - AML HHE 1996092 402 -1 n -0 90 90 - AML HHE 1992240 192 1993239 n -0 90 90 - AML HHE 1993240 249 1993304 n -0 90 90 - AML HHE 1993305 303 1994241 n -0 90 90 - AML HHE 1991244 123 1992239 n -0 90 90 - AML HHN 1994242 350 1996091 n -0 0 90 - AML HHN 1993305 302 1994241 n -0 0 90 - AML HHN 1991244 122 1992239 n -0 0 90 - AML HHN 1996092 401 -1 n -0 0 90 - AML HHN 1993240 248 1993304 n -0 0 90 - AML HHN 1992240 191 1993239 n -0 0 90 - AML HHZ 1992240 190 1993239 n -0 0 0 - AML HHZ 1993240 247 1993304 n -0 0 0 - AML HHZ 1993305 301 1994241 n -0 0 0 - AML HHZ 1994242 349 1996091 n -0 0 0 - AML HHZ 1991244 121 1992239 n -0 0 0 - AML HHZ 1996092 400 -1 n -0 0 0 - AML HLE 1993305 306 1994241 n -0 90 90 - AML HLE 1991244 126 1992239 n -0 90 90 - AML HLE 1992240 189 1993239 n -0 90 90 - AML HLE 1993240 252 1993304 n -0 90 90 - AML HLE 1994242 354 1995006 n -0 90 90 - AML HLN 1991244 125 1992239 n -0 0 90 - AML HLN 1992240 188 1993239 n -0 0 90 - AML HLN 1993240 251 1993304 n -0 0 90 - AML HLN 1994242 353 1995006 n -0 0 90 - AML HLN 1993305 305 1994241 n -0 0 90 - AML HLZ 1991244 124 1992239 n -0 0 0 - AML HLZ 1994242 352 1995006 n -0 0 0 - AML HLZ 1992240 187 1993239 n -0 0 0 - AML HLZ 1993240 250 1993304 n -0 0 0 - AML HLZ 1993305 304 1994241 n -0 0 0 - AML LHE 1998160 726 -1 n -0 90 90 - AML LHN 1998160 725 -1 n -0 0 90 - AML LHZ 1998160 724 -1 n -0 0 0 - ANA BHE 1997271 18 2001365 n -0 90 90 - ANA BHN 1997271 17 2001365 n -0 0 90 - ANA BHZ 1997271 16 2001365 n -0 0 0 - ARA BHE 1999174 69 2001365 n -0 90 90 - ARA BHN 1999174 68 2001365 n -0 0 90 - ARA BHZ 1999174 67 2001365 n -0 0 0 - ATUS BHE 1997271 27 2001365 n -0 90 90 - ATUS BHN 1997271 26 2001365 n -0 0 90 - ATUS BHZ 1997271 25 2001365 n -0 0 0 - BAY HHE 1998236 778 -1 n 0 90 90 - BAY HHE 1997190 769 1998235 n 0 90 90 - BAY HHN 1997190 770 1998235 n 0 0 90 - BAY HHN 1998236 779 -1 n 0 0 90 - BAY HHZ 1997190 771 1998235 n 0 0 0 - BAY HHZ 1998236 780 -1 n 0 0 0 - BCHU BHE 1997271 30 2001365 n -0 90 90 - BCHU BHN 1997271 29 2001365 n -0 0 90 - BCHU BHZ 1997271 28 2001365 n -0 0 0 - BGK2 BHE 1992240 459 1992261 n -0 90 90 - BGK2 BHE 1991244 429 1992239 n -0 90 90 - BGK2 BHE 1993240 528 1993253 n -0 90 90 - BGK2 BHN 1993240 527 1993253 n -0 0 90 - BGK2 BHN 1992240 458 1992261 n -0 0 90 - BGK2 BHN 1991244 428 1992239 n -0 0 90 - BGK2 BHZ 1992240 457 1992261 n -0 0 0 - BGK2 BHZ 1993240 526 1993253 n -0 0 0 - BGK2 BHZ 1991244 427 1992239 n -0 0 0 - BGK2 BLE 1992261 489 1993239 n -0 90 90 - BGK2 BLE 1993240 531 1993253 n -0 90 90 - BGK2 BLN 1992261 488 1993239 n -0 0 90 - BGK2 BLN 1993240 530 1993253 n -0 0 90 - BGK2 BLZ 1992261 487 1993239 n -0 0 0 - BGK2 BLZ 1993240 529 1993253 n -0 0 0 - BGK2 HHE 1992240 180 1993239 n -0 90 90 - BGK2 HHE 1991244 117 1992239 n -0 90 90 - BGK2 HHE 1993240 237 1993253 n -0 90 90 - BGK2 HHN 1992240 179 1993239 n -0 0 90 - BGK2 HHN 1993240 236 1993253 n -0 0 90 - BGK2 HHN 1991244 116 1992239 n -0 0 90 - BGK2 HHZ 1992240 178 1993239 n -0 0 0 - BGK2 HHZ 1993240 235 1993253 n -0 0 0 - BGK2 HHZ 1991244 115 1992239 n -0 0 0 - BGK2 HLE 1992240 177 1993239 n -0 90 90 - BGK2 HLE 1991244 120 1992239 n -0 90 90 - BGK2 HLE 1993240 240 1993253 n -0 90 90 - BGK2 HLN 1991244 119 1992239 n -0 0 90 - BGK2 HLN 1993240 239 1993253 n -0 0 90 - BGK2 HLN 1992240 176 1993239 n -0 0 90 - BGK2 HLZ 1991244 118 1992239 n -0 0 0 - BGK2 HLZ 1992240 175 1993239 n -0 0 0 - BGK2 HLZ 1993240 238 1993253 n -0 0 0 - BRVK BHE 1994244 811 -1 - 0.015 90 90 Station Maintenance. Tests may be in progress. BRVK BHN 1994244 812 -1 - 0.015 0 90 Station Maintenance. Tests may be in progress. BRVK BHZ 1994244 813 -1 - 0.015 0 0 Station Maintenance. Tests may be in progress. BRVK BLE 1994244 814 -1 - 0.015 90 90 NRTS data inserted into field tape data gaps, time BRVK BLN 1994244 815 -1 - 0.015 0 90 NRTS data inserted into field tape data gaps, time BRVK BLZ 1994244 816 -1 - 0.015 0 0 NRTS data inserted into field tape data gaps, time CHAT BHE 1999195 72 2001365 n -0 90 90 - CHAT BHN 1999195 71 2001365 n -0 0 90 - CHAT BHZ 1999195 70 2001365 n -0 0 0 - CHK BHE 1994204 745 -1 n 0 90 90 - CHK BHN 1994204 746 -1 n 0 0 90 - CHK BHZ 1994204 747 -1 n 0 0 0 - CHK HHE 1994204 748 -1 n 0 90 90 - CHK HHN 1994204 749 -1 n 0 0 90 - CHK HHZ 1994204 750 -1 n 0 0 0 - CHKZ BHE 1996015 793 -1 n 0 90 90 - CHKZ BHN 1996015 794 -1 n 0 0 90 - CHKZ BHZ 1996015 795 -1 n 0 0 0 - CHM BHE 1992240 450 1992261 n -0 90 90 - CHM BHE 1994242 618 1996091 n -0 90 90 - CHM BHE 1996092 678 -1 n -0 90 90 - CHM BHE 1993240 510 1993304 n -0 90 90 - CHM BHE 1993305 570 1994241 n -0 90 90 - CHM BHE 1991244 420 1992239 n -0 90 90 - CHM BHN 1994242 617 1996091 n -0 0 90 - CHM BHN 1996092 677 -1 n -0 0 90 - CHM BHN 1993305 569 1994241 n -0 0 90 - CHM BHN 1993240 509 1993304 n -0 0 90 - CHM BHN 1992240 449 1992261 n -0 0 90 - CHM BHN 1991244 419 1992239 n -0 0 90 - CHM BHZ 1994242 616 1996091 n -0 0 0 - CHM BHZ 1993240 508 1993304 n -0 0 0 - CHM BHZ 1993305 568 1994241 n -0 0 0 - CHM BHZ 1996092 676 -1 n -0 0 0 - CHM BHZ 1991244 418 1992239 n -0 0 0 - CHM BHZ 1992240 448 1992261 n -0 0 0 - CHM BLE 1993305 573 1994241 n -0 90 90 - CHM BLE 1992261 480 1993239 n -0 90 90 - CHM BLE 1993240 513 1993304 n -0 90 90 - CHM BLE 1994242 621 1995005 n -0 90 90 - CHM BLN 1993305 572 1994241 n -0 0 90 - CHM BLN 1993240 512 1993304 n -0 0 90 - CHM BLN 1994242 620 1995005 n -0 0 90 - CHM BLN 1992261 479 1993239 n -0 0 90 - CHM BLZ 1993305 571 1994241 n -0 0 0 - CHM BLZ 1992261 478 1993239 n -0 0 0 - CHM BLZ 1993240 511 1993304 n -0 0 0 - CHM BLZ 1994242 619 1995005 n -0 0 0 - CHM HHE 1991244 99 1992239 n -0 90 90 - CHM HHE 1996092 387 -1 n -0 90 90 - CHM HHE 1993240 219 1993304 n -0 90 90 - CHM HHE 1993305 279 1994241 n -0 90 90 - CHM HHE 1992240 162 1993239 n -0 90 90 - CHM HHE 1994242 327 1996091 n -0 90 90 - CHM HHN 1993240 218 1993304 n -0 0 90 - CHM HHN 1996092 386 -1 n -0 0 90 - CHM HHN 1992240 161 1993239 n -0 0 90 - CHM HHN 1991244 98 1992239 n -0 0 90 - CHM HHN 1994242 326 1996091 n -0 0 90 - CHM HHN 1993305 278 1994241 n -0 0 90 - CHM HHZ 1991244 97 1992239 n -0 0 0 - CHM HHZ 1996092 385 -1 n -0 0 0 - CHM HHZ 1993240 217 1993304 n -0 0 0 - CHM HHZ 1994242 325 1996091 n -0 0 0 - CHM HHZ 1993305 277 1994241 n -0 0 0 - CHM HHZ 1992240 160 1993239 n -0 0 0 - CHM HLE 1991244 102 1992239 n -0 90 90 - CHM HLE 1992240 159 1993239 n -0 90 90 - CHM HLE 1993305 282 1994241 n -0 90 90 - CHM HLE 1993240 222 1993304 n -0 90 90 - CHM HLE 1994242 330 1995006 n -0 90 90 - CHM HLN 1993240 221 1993304 n -0 0 90 - CHM HLN 1992240 158 1993239 n -0 0 90 - CHM HLN 1991244 101 1992239 n -0 0 90 - CHM HLN 1993305 281 1994241 n -0 0 90 - CHM HLN 1994242 329 1995006 n -0 0 90 - CHM HLZ 1993305 280 1994241 n -0 0 0 - CHM HLZ 1993240 220 1993304 n -0 0 0 - CHM HLZ 1991244 100 1992239 n -0 0 0 - CHM HLZ 1994242 328 1995006 n -0 0 0 - CHM HLZ 1992240 157 1993239 n -0 0 0 - CHM LHE 1998160 711 -1 n -0 90 90 - CHM LHN 1998160 710 -1 n -0 0 90 - CHM LHZ 1998160 709 -1 n -0 0 0 - DGE BHE 1998249 39 2001365 n -0 90 90 - DGE BHN 1998249 38 2001365 n -0 0 90 - DGE BHZ 1998249 37 2001365 n -0 0 0 - EKS2 BHE 1991244 423 1992239 n -0 90 90 - EKS2 BHE 1992240 453 1992261 n -0 90 90 - EKS2 BHE 1994242 633 1996091 n -0 90 90 - EKS2 BHE 1996092 690 -1 n -0 90 90 - EKS2 BHE 1993240 516 1993304 n -0 90 90 - EKS2 BHE 1993305 576 1994241 n -0 90 90 - EKS2 BHN 1996092 689 -1 n -0 0 90 - EKS2 BHN 1992240 452 1992261 n -0 0 90 - EKS2 BHN 1994242 632 1996091 n -0 0 90 - EKS2 BHN 1991244 422 1992239 n -0 0 90 - EKS2 BHN 1993305 575 1994241 n -0 0 90 - EKS2 BHN 1993240 515 1993304 n -0 0 90 - EKS2 BHZ 1993240 514 1993304 n -0 0 0 - EKS2 BHZ 1992240 451 1992261 n -0 0 0 - EKS2 BHZ 1994242 631 1996091 n -0 0 0 - EKS2 BHZ 1991244 421 1992239 n -0 0 0 - EKS2 BHZ 1993305 574 1994241 n -0 0 0 - EKS2 BHZ 1996092 688 -1 n -0 0 0 - EKS2 BLE 1994242 630 1995005 n -0 90 90 - EKS2 BLE 1993240 519 1993304 n -0 90 90 - EKS2 BLE 1993305 579 1994241 n -0 90 90 - EKS2 BLE 1992261 483 1993239 n -0 90 90 - EKS2 BLN 1992261 482 1993239 n -0 0 90 - EKS2 BLN 1993305 578 1994241 n -0 0 90 - EKS2 BLN 1994242 629 1995005 n -0 0 90 - EKS2 BLN 1993240 518 1993304 n -0 0 90 - EKS2 BLZ 1993305 577 1994241 n -0 0 0 - EKS2 BLZ 1993240 517 1993304 n -0 0 0 - EKS2 BLZ 1994242 628 1995005 n -0 0 0 - EKS2 BLZ 1992261 481 1993239 n -0 0 0 - EKS2 HHE 1993305 285 1994241 n -0 90 90 - EKS2 HHE 1996092 399 -1 n -0 90 90 - EKS2 HHE 1992240 168 1993239 n -0 90 90 - EKS2 HHE 1991244 105 1992239 n -0 90 90 - EKS2 HHE 1994242 342 1996091 n -0 90 90 - EKS2 HHE 1993240 225 1993304 n -0 90 90 - EKS2 HHN 1996092 398 -1 n -0 0 90 - EKS2 HHN 1992240 167 1993239 n -0 0 90 - EKS2 HHN 1993240 224 1993304 n -0 0 90 - EKS2 HHN 1991244 104 1992239 n -0 0 90 - EKS2 HHN 1993305 284 1994241 n -0 0 90 - EKS2 HHN 1994242 341 1996091 n -0 0 90 - EKS2 HHZ 1993240 223 1993304 n -0 0 0 - EKS2 HHZ 1991244 103 1992239 n -0 0 0 - EKS2 HHZ 1996092 397 -1 n -0 0 0 - EKS2 HHZ 1992240 166 1993239 n -0 0 0 - EKS2 HHZ 1993305 283 1994241 n -0 0 0 - EKS2 HHZ 1994242 340 1996091 n -0 0 0 - EKS2 HLE 1991244 108 1992239 n -0 90 90 - EKS2 HLE 1994242 339 1995006 n -0 90 90 - EKS2 HLE 1993240 228 1993304 n -0 90 90 - EKS2 HLE 1993305 288 1994241 n -0 90 90 - EKS2 HLE 1992240 165 1993239 n -0 90 90 - EKS2 HLN 1993240 227 1993304 n -0 0 90 - EKS2 HLN 1992240 164 1993239 n -0 0 90 - EKS2 HLN 1991244 107 1992239 n -0 0 90 - EKS2 HLN 1993305 287 1994241 n -0 0 90 - EKS2 HLN 1994242 338 1995006 n -0 0 90 - EKS2 HLZ 1993240 226 1993304 n -0 0 0 - EKS2 HLZ 1991244 106 1992239 n -0 0 0 - EKS2 HLZ 1994242 337 1995006 n -0 0 0 - EKS2 HLZ 1993305 286 1994241 n -0 0 0 - EKS2 HLZ 1992240 163 1993239 n -0 0 0 - EKS2 LHE 1998160 723 -1 n -0 90 90 - EKS2 LHN 1998160 722 -1 n -0 0 90 - EKS2 LHZ 1998160 721 -1 n -0 0 0 - ERPT BHE 1999220 708 2000165 n -0 90 90 - ERPT BHN 1999220 707 2000165 n -0 0 90 - ERPT BHZ 1999220 706 2000165 n -0 0 0 - ERPT HHE 1999220 417 2000165 n -0 90 90 - ERPT HHN 1999220 416 2000165 n -0 0 90 - ERPT HHZ 1999220 415 2000165 n -0 0 0 - ERPT LHE 1999220 741 2000165 n -0 90 90 - ERPT LHN 1999220 740 2000165 n -0 0 90 - ERPT LHZ 1999220 739 2000165 n -0 0 0 - HARA BHE 1999174 66 2001365 n -0 90 90 - HARA BHN 1999174 65 2001365 n -0 0 90 - HARA BHZ 1999174 64 2001365 n -0 0 0 - HLQI BHE 1999163 54 2001365 n -0 90 90 - HLQI BHN 1999163 53 2001365 n -0 0 90 - HLQI BHZ 1999163 52 2001365 n -0 0 0 - KAI BHE 1998249 42 2001365 n -0 90 90 - KAI BHN 1998249 41 2001365 n -0 0 90 - KAI BHZ 1998249 40 2001365 n -0 0 0 - KAR BHE 1997271 12 2001365 n -0 90 90 - KAR BHN 1997271 11 2001365 n -0 0 90 - KAR BHZ 1997271 10 2001365 n -0 0 0 - KARL BHE 1999218 84 2001365 n -0 90 90 - KARL BHN 1999218 83 2001365 n -0 0 90 - KARL BHZ 1999218 82 2001365 n -0 0 0 - KASH BHE 1997271 33 2001365 n -0 90 90 - KASH BHN 1997271 32 2001365 n -0 0 90 - KASH BHZ 1997271 31 2001365 n -0 0 0 - KAZ BHE 1997271 21 2001365 n -0 90 90 - KAZ BHN 1997271 20 2001365 n -0 0 90 - KAZ BHZ 1997271 19 2001365 n -0 0 0 - KBK BHE 1991244 441 1992239 n -0 90 90 - KBK BHE 1992240 474 1992261 n -0 90 90 - KBK BHE 1996092 702 -1 n -0 90 90 - KBK BHE 1993240 558 1993304 n -0 90 90 - KBK BHE 1994242 654 1996091 n -0 90 90 - KBK BHE 1993305 606 1994073 n -0 90 90 - KBK BHN 1993240 557 1993304 n -0 0 90 - KBK BHN 1991244 440 1992239 n -0 0 90 - KBK BHN 1993305 605 1994073 n -0 0 90 - KBK BHN 1994242 653 1996091 n -0 0 90 - KBK BHN 1996092 701 -1 n -0 0 90 - KBK BHN 1992240 473 1992261 n -0 0 90 - KBK BHZ 1991244 439 1992239 n -0 0 0 - KBK BHZ 1994242 652 1996091 n -0 0 0 - KBK BHZ 1996092 700 -1 n -0 0 0 - KBK BHZ 1992240 472 1992261 n -0 0 0 - KBK BHZ 1993305 604 1994073 n -0 0 0 - KBK BHZ 1993240 556 1993304 n -0 0 0 - KBK BLE 1993305 609 1994073 n -0 90 90 - KBK BLE 1992261 504 1993239 n -0 90 90 - KBK BLE 1994242 657 1995005 n -0 90 90 - KBK BLE 1993240 561 1993304 n -0 90 90 - KBK BLN 1994242 656 1995005 n -0 0 90 - KBK BLN 1993240 560 1993304 n -0 0 90 - KBK BLN 1992261 503 1993239 n -0 0 90 - KBK BLN 1993305 608 1994073 n -0 0 90 - KBK BLZ 1994242 655 1995005 n -0 0 0 - KBK BLZ 1993240 559 1993304 n -0 0 0 - KBK BLZ 1993305 607 1994073 n -0 0 0 - KBK BLZ 1992261 502 1993239 n -0 0 0 - KBK HHE 1991244 141 1992239 n -0 90 90 - KBK HHE 1996092 411 -1 n -0 90 90 - KBK HHE 1993240 267 1993304 n -0 90 90 - KBK HHE 1993305 315 1994073 n -0 90 90 - KBK HHE 1994242 363 1996091 n -0 90 90 - KBK HHE 1992240 210 1993239 n -0 90 90 - KBK HHN 1996092 410 -1 n -0 0 90 - KBK HHN 1993305 314 1994073 n -0 0 90 - KBK HHN 1993240 266 1993304 n -0 0 90 - KBK HHN 1992240 209 1993239 n -0 0 90 - KBK HHN 1991244 140 1992239 n -0 0 90 - KBK HHN 1994242 362 1996091 n -0 0 90 - KBK HHZ 1993305 313 1994073 n -0 0 0 - KBK HHZ 1993240 265 1993304 n -0 0 0 - KBK HHZ 1992240 208 1993239 n -0 0 0 - KBK HHZ 1991244 139 1992239 n -0 0 0 - KBK HHZ 1994242 361 1996091 n -0 0 0 - KBK HHZ 1996092 409 -1 n -0 0 0 - KBK HLE 1993240 270 1993304 n -0 90 90 - KBK HLE 1993305 318 1994073 n -0 90 90 - KBK HLE 1994242 366 1995006 n -0 90 90 - KBK HLE 1991244 144 1992239 n -0 90 90 - KBK HLE 1992240 207 1993239 n -0 90 90 - KBK HLN 1991244 143 1992239 n -0 0 90 - KBK HLN 1993305 317 1994073 n -0 0 90 - KBK HLN 1993240 269 1993304 n -0 0 90 - KBK HLN 1992240 206 1993239 n -0 0 90 - KBK HLN 1994242 365 1995006 n -0 0 90 - KBK HLZ 1992240 205 1993239 n -0 0 0 - KBK HLZ 1993305 316 1994073 n -0 0 0 - KBK HLZ 1994242 364 1995006 n -0 0 0 - KBK HLZ 1991244 142 1992239 n -0 0 0 - KBK HLZ 1993240 268 1993304 n -0 0 0 - KBK LHE 1998160 735 -1 n -0 90 90 - KBK LHN 1998160 734 -1 n -0 0 90 - KBK LHZ 1998160 733 -1 n -0 0 0 - KDJ BHE 1997271 9 2001365 n -0 90 90 - KDJ BHN 1997271 8 2001365 n -0 0 90 - KDJ BHZ 1997271 7 2001365 n -0 0 0 - KENS BHE 1999218 81 2001365 n -0 90 90 - KENS BHN 1999218 80 2001365 n -0 0 90 - KENS BHZ 1999218 79 2001365 n -0 0 0 - KHA BHE 1997271 6 2001365 n -0 90 90 - KHA BHN 1997271 5 2001365 n -0 0 90 - KHA BHZ 1997271 4 2001365 n -0 0 0 - KKL HHE 1997190 781 -1 n 0 90 90 - KKL HHN 1997190 782 -1 n 0 0 90 - KKL HHZ 1997190 783 -1 n 0 0 0 - KOPG BHE 1999163 57 2001365 n -0 90 90 - KOPG BHN 1999163 56 2001365 n -0 0 90 - KOPG BHZ 1999163 55 2001365 n -0 0 0 - KSA BHE 1997271 24 2001365 n -0 90 90 - KSA BHN 1997271 23 2001365 n -0 0 90 - KSA BHZ 1997271 22 2001365 n -0 0 0 - KUR BHE 1994206 766 -1 n 0.025 90 90 - KUR BHN 1994206 767 -1 n 0.025 0 90 - KUR BHZ 1994206 768 -1 n 0.025 0 0 - KUR HHE 1998233 772 1998235 n 0.025 90 90 - KUR HHE 1997186 751 1997273 n 0 90 90 - KUR HHE 1998259 784 -1 n 0.025 90 90 - KUR HHN 1997186 752 1997273 n 0 0 90 - KUR HHN 1998259 785 -1 n 0.025 0 90 - KUR HHN 1998233 773 1998235 n 0.025 0 90 - KUR HHZ 1997186 753 1997273 n 0 0 0 - KUR HHZ 1998259 786 -1 n 0.025 0 0 - KUR HHZ 1998233 774 1998235 n 0.025 0 0 - KUR SHE 1994206 802 -1 n 0 90 90 - KUR SHN 1994206 803 -1 n 0 0 90 - KUR SHZ 1994206 804 -1 n 0 0 0 - KURK BHE 1996330 796 -1 n 0 90 90 - KURK BHN 1996330 797 -1 n 0 0 90 - KURK BHZ 1996330 798 -1 n 0 0 0 - KURK SHE 1996330 805 -1 n 0 90 90 - KURK SHN 1996330 806 -1 n 0 0 90 - KURK SHZ 1996330 807 -1 n 0 0 0 - KZA BHE 1991244 435 1992239 n -0 90 90 - KZA BHE 1993240 546 1993263 n -0 90 90 - KZA BHE 1994242 648 1996091 n -0 90 90 - KZA BHE 1992240 468 1992261 n -0 90 90 - KZA BHE 1996092 696 -1 n -0 90 90 - KZA BHN 1994242 647 1996091 n -0 0 90 - KZA BHN 1996092 695 -1 n -0 0 90 - KZA BHN 1992240 467 1992261 n -0 0 90 - KZA BHN 1993240 545 1993263 n -0 0 90 - KZA BHN 1991244 434 1992239 n -0 0 90 - KZA BHZ 1991244 433 1992239 n -0 0 0 - KZA BHZ 1992240 466 1992261 n -0 0 0 - KZA BHZ 1993240 544 1993263 n -0 0 0 - KZA BHZ 1994242 646 1996091 n -0 0 0 - KZA BHZ 1996092 694 -1 n -0 0 0 - KZA BLE 1992261 498 1993239 n -0 90 90 - KZA BLE 1994242 651 1995005 n -0 90 90 - KZA BLE 1993240 549 1993263 n -0 90 90 - KZA BLN 1992261 497 1993239 n -0 0 90 - KZA BLN 1993240 548 1993263 n -0 0 90 - KZA BLN 1994242 650 1995005 n -0 0 90 - KZA BLZ 1993240 547 1993263 n -0 0 0 - KZA BLZ 1994242 649 1995005 n -0 0 0 - KZA BLZ 1992261 496 1993239 n -0 0 0 - KZA HHE 1994242 357 1996091 n -0 90 90 - KZA HHE 1993240 255 1993263 n -0 90 90 - KZA HHE 1991244 129 1992239 n -0 90 90 - KZA HHE 1996092 405 -1 n -0 90 90 - KZA HHE 1992240 198 1993239 n -0 90 90 - KZA HHN 1994242 356 1996091 n -0 0 90 - KZA HHN 1993240 254 1993263 n -0 0 90 - KZA HHN 1991244 128 1992239 n -0 0 90 - KZA HHN 1992240 197 1993239 n -0 0 90 - KZA HHN 1996092 404 -1 n -0 0 90 - KZA HHZ 1993240 253 1993263 n -0 0 0 - KZA HHZ 1996092 403 -1 n -0 0 0 - KZA HHZ 1994242 355 1996091 n -0 0 0 - KZA HHZ 1992240 196 1993239 n -0 0 0 - KZA HHZ 1991244 127 1992239 n -0 0 0 - KZA HLE 1991244 132 1992239 n -0 90 90 - KZA HLE 1993240 258 1993263 n -0 90 90 - KZA HLE 1994242 360 1995006 n -0 90 90 - KZA HLE 1992240 195 1993239 n -0 90 90 - KZA HLN 1992240 194 1993239 n -0 0 90 - KZA HLN 1991244 131 1992239 n -0 0 90 - KZA HLN 1993240 257 1993263 n -0 0 90 - KZA HLN 1994242 359 1995006 n -0 0 90 - KZA HLZ 1994242 358 1995006 n -0 0 0 - KZA HLZ 1993240 256 1993263 n -0 0 0 - KZA HLZ 1991244 130 1992239 n -0 0 0 - KZA HLZ 1992240 193 1993239 n -0 0 0 - KZA LHE 1998160 729 -1 n -0 90 90 - KZA LHN 1998160 728 -1 n -0 0 90 - KZA LHZ 1998160 727 -1 n -0 0 0 - MAK HHE 1998234 85 -1 - 0 90 90 SN#119547 MAK HHN 1998234 86 -1 - 0 0 90 SN#119547 MAK HHZ 1998234 87 -1 - 0 0 0 SN#119547 MAKZ BHE 1996258 88 -1 - 0.033 90 90 MAKZ BHN 1996258 89 -1 - 0.033 0 90 MAKZ BHZ 1996258 90 -1 - 0.033 0 0 MAKZ SHE 1996258 91 -1 - 0.033 90 90 MAKZ SHN 1996258 92 -1 - 0.033 0 90 MAKZ SHZ 1996258 93 -1 - 0.033 0 0 NRN BHE 1997271 15 2001365 n -0 90 90 - NRN BHN 1997271 14 2001365 n -0 0 90 - NRN BHZ 1997271 13 2001365 n -0 0 0 - PDG BHE 1997271 3 2001365 n -0 90 90 - PDG BHN 1997271 2 2001365 n -0 0 90 - PDG BHZ 1997271 1 2001365 n -0 0 0 - PIQG BHE 1999171 63 2001365 n -0 90 90 - PIQG BHN 1999171 62 2001365 n -0 0 90 - PIQG BHZ 1999171 61 2001365 n -0 0 0 - POGR BHE 1999195 75 2001365 n -0 90 90 - POGR BHN 1999195 74 2001365 n -0 0 90 - POGR BHZ 1999195 73 2001365 n -0 0 0 - TERE BHE 1999195 78 2001365 n -0 90 90 - TERE BHN 1999195 77 2001365 n -0 0 90 - TERE BHZ 1999195 76 2001365 n -0 0 0 - TGMT BHE 1999170 60 2001365 n -0 90 90 - TGMT BHN 1999170 59 2001365 n -0 0 90 - TGMT BHZ 1999170 58 2001365 n -0 0 0 - TKM BHE 1993240 552 1993304 n -0 90 90 - TKM BHE 1992240 471 1992261 n -0 90 90 - TKM BHE 1993305 600 1994241 n -0 90 90 - TKM BHE 1991244 438 1992239 n -0 90 90 - TKM BHN 1993240 551 1993304 n -0 0 90 - TKM BHN 1992240 470 1992261 n -0 0 90 - TKM BHN 1993305 599 1994241 n -0 0 90 - TKM BHN 1991244 437 1992239 n -0 0 90 - TKM BHZ 1993305 598 1994241 n -0 0 0 - TKM BHZ 1992240 469 1992261 n -0 0 0 - TKM BHZ 1993240 550 1993304 n -0 0 0 - TKM BHZ 1991244 436 1992239 n -0 0 0 - TKM BLE 1993240 555 1993304 n -0 90 90 - TKM BLE 1993305 603 1994241 n -0 90 90 - TKM BLE 1992261 501 1993239 n -0 90 90 - TKM BLN 1993305 602 1994241 n -0 0 90 - TKM BLN 1993240 554 1993304 n -0 0 90 - TKM BLN 1992261 500 1993239 n -0 0 90 - TKM BLZ 1993240 553 1993304 n -0 0 0 - TKM BLZ 1992261 499 1993239 n -0 0 0 - TKM BLZ 1993305 601 1994241 n -0 0 0 - TKM HHE 1993305 309 1994241 n -0 90 90 - TKM HHE 1992240 204 1993239 n -0 90 90 - TKM HHE 1993240 261 1993304 n -0 90 90 - TKM HHE 1991244 135 1992239 n -0 90 90 - TKM HHN 1991244 134 1992239 n -0 0 90 - TKM HHN 1993305 308 1994241 n -0 0 90 - TKM HHN 1993240 260 1993304 n -0 0 90 - TKM HHN 1992240 203 1993239 n -0 0 90 - TKM HHZ 1993240 259 1993304 n -0 0 0 - TKM HHZ 1991244 133 1992239 n -0 0 0 - TKM HHZ 1992240 202 1993239 n -0 0 0 - TKM HHZ 1993305 307 1994241 n -0 0 0 - TKM HLE 1993305 312 1994241 n -0 90 90 - TKM HLE 1992240 201 1993239 n -0 90 90 - TKM HLE 1991244 138 1992239 n -0 90 90 - TKM HLE 1993240 264 1993304 n -0 90 90 - TKM HLN 1992240 200 1993239 n -0 0 90 - TKM HLN 1993240 263 1993304 n -0 0 90 - TKM HLN 1993305 311 1994241 n -0 0 90 - TKM HLN 1991244 137 1992239 n -0 0 90 - TKM HLZ 1991244 136 1992239 n -0 0 0 - TKM HLZ 1992240 199 1993239 n -0 0 0 - TKM HLZ 1993240 262 1993304 n -0 0 0 - TKM HLZ 1993305 310 1994241 n -0 0 0 - TKM2 BHE 1996092 699 -1 n -0 90 90 - TKM2 BHE 1994257 672 1996091 n -0 90 90 - TKM2 BHN 1996092 698 -1 n -0 0 90 - TKM2 BHN 1994257 671 1996091 n -0 0 90 - TKM2 BHZ 1994257 670 1996091 n -0 0 0 - TKM2 BHZ 1996092 697 -1 n -0 0 0 - TKM2 BLE 1994257 675 1995005 n -0 90 90 - TKM2 BLN 1994257 674 1995005 n -0 0 90 - TKM2 BLZ 1994257 673 1995005 n -0 0 0 - TKM2 HHE 1994257 381 1996091 n -0 90 90 - TKM2 HHE 1996092 408 -1 n -0 90 90 - TKM2 HHN 1994257 380 1996091 n -0 0 90 - TKM2 HHN 1996092 407 -1 n -0 0 90 - TKM2 HHZ 1994257 379 1996091 n -0 0 0 - TKM2 HHZ 1996092 406 -1 n -0 0 0 - TKM2 HLE 1994257 384 1995006 n -0 90 90 - TKM2 HLN 1994257 383 1995006 n -0 0 90 - TKM2 HLZ 1994257 382 1995006 n -0 0 0 - TKM2 LHE 1998160 732 -1 n -0 90 90 - TKM2 LHN 1998160 731 -1 n -0 0 90 - TKM2 LHZ 1998160 730 -1 n -0 0 0 - TLG BHE 1997280 94 -1 - 0 90 90 SN#T345 TLG BHN 1997280 95 -1 - 0 0 90 SN#T345 TLG BHZ 1997248 96 -1 - 0 0 0 SN#T345 UCH BHE 1994242 624 1996091 n -0 90 90 - UCH BHE 1992240 462 1992261 n -0 90 90 - UCH BHE 1991244 447 1992239 n -0 90 90 - UCH BHE 1996092 681 -1 n -0 90 90 - UCH BHE 1993240 534 1993304 n -0 90 90 - UCH BHE 1993305 588 1994241 n -0 90 90 - UCH BHN 1994242 623 1996091 n -0 0 90 - UCH BHN 1993305 587 1994241 n -0 0 90 - UCH BHN 1992240 461 1992261 n -0 0 90 - UCH BHN 1993240 533 1993304 n -0 0 90 - UCH BHN 1996092 680 -1 n -0 0 90 - UCH BHN 1991244 446 1992239 n -0 0 90 - UCH BHZ 1993240 532 1993304 n -0 0 0 - UCH BHZ 1993305 586 1994241 n -0 0 0 - UCH BHZ 1992240 460 1992261 n -0 0 0 - UCH BHZ 1994242 622 1996091 n -0 0 0 - UCH BHZ 1996092 679 -1 n -0 0 0 - UCH BHZ 1991244 445 1992239 n -0 0 0 - UCH BLE 1993305 591 1994241 n -0 90 90 - UCH BLE 1993240 537 1993304 n -0 90 90 - UCH BLE 1994242 627 1995005 n -0 90 90 - UCH BLE 1992261 492 1993239 n -0 90 90 - UCH BLN 1993305 590 1994241 n -0 0 90 - UCH BLN 1993240 536 1993304 n -0 0 90 - UCH BLN 1994242 626 1995005 n -0 0 90 - UCH BLN 1992261 491 1993239 n -0 0 90 - UCH BLZ 1993305 589 1994241 n -0 0 0 - UCH BLZ 1992261 490 1993239 n -0 0 0 - UCH BLZ 1994242 625 1995005 n -0 0 0 - UCH BLZ 1993240 535 1993304 n -0 0 0 - UCH HHE 1992240 186 1993239 n -0 90 90 - UCH HHE 1996092 390 -1 n -0 90 90 - UCH HHE 1994242 333 1996091 n -0 90 90 - UCH HHE 1993305 297 1994241 n -0 90 90 - UCH HHE 1991244 153 1992239 n -0 90 90 - UCH HHE 1993240 243 1993304 n -0 90 90 - UCH HHN 1991244 152 1992239 n -0 0 90 - UCH HHN 1993240 242 1993304 n -0 0 90 - UCH HHN 1996092 389 -1 n -0 0 90 - UCH HHN 1992240 185 1993239 n -0 0 90 - UCH HHN 1993305 296 1994241 n -0 0 90 - UCH HHN 1994242 332 1996091 n -0 0 90 - UCH HHZ 1991244 151 1992239 n -0 0 0 - UCH HHZ 1993305 295 1994241 n -0 0 0 - UCH HHZ 1992240 184 1993239 n -0 0 0 - UCH HHZ 1994242 331 1996091 n -0 0 0 - UCH HHZ 1996092 388 -1 n -0 0 0 - UCH HHZ 1993240 241 1993304 n -0 0 0 - UCH HLE 1994242 336 1995006 n -0 90 90 - UCH HLE 1993305 300 1994241 n -0 90 90 - UCH HLE 1991244 156 1992239 n -0 90 90 - UCH HLE 1993240 246 1993304 n -0 90 90 - UCH HLE 1992240 183 1993239 n -0 90 90 - UCH HLN 1993240 245 1993304 n -0 0 90 - UCH HLN 1994242 335 1995006 n -0 0 90 - UCH HLN 1992240 182 1993239 n -0 0 90 - UCH HLN 1993305 299 1994241 n -0 0 90 - UCH HLN 1991244 155 1992239 n -0 0 90 - UCH HLZ 1991244 154 1992239 n -0 0 0 - UCH HLZ 1993305 298 1994241 n -0 0 0 - UCH HLZ 1994242 334 1995006 n -0 0 0 - UCH HLZ 1993240 244 1993304 n -0 0 0 - UCH HLZ 1992240 181 1993239 n -0 0 0 - UCH LHE 1998160 714 -1 n -0 90 90 - UCH LHN 1998160 713 -1 n -0 0 90 - UCH LHZ 1998160 712 -1 n -0 0 0 - ULHL BHE 1994252 666 1996091 n -0 90 90 - ULHL BHE 1996092 687 -1 n -0 90 90 - ULHL BHN 1994252 665 1996091 n -0 0 90 - ULHL BHN 1996092 686 -1 n -0 0 90 - ULHL BHZ 1994252 664 1996091 n -0 0 0 - ULHL BHZ 1996092 685 -1 n -0 0 0 - ULHL BLE 1994252 669 1995005 n -0 90 90 - ULHL BLN 1994252 668 1995005 n -0 0 90 - ULHL BLZ 1994252 667 1995005 n -0 0 0 - ULHL HHE 1994252 375 1996091 n -0 90 90 - ULHL HHE 1996092 396 -1 n -0 90 90 - ULHL HHN 1996092 395 -1 n -0 0 90 - ULHL HHN 1994252 374 1996091 n -0 0 90 - ULHL HHZ 1994252 373 1996091 n -0 0 0 - ULHL HHZ 1996092 394 -1 n -0 0 0 - ULHL HLE 1994252 378 1995006 n -0 90 90 - ULHL HLN 1994252 377 1995006 n -0 0 90 - ULHL HLZ 1994252 376 1995006 n -0 0 0 - ULHL LHE 1998160 720 -1 n -0 90 90 - ULHL LHN 1998160 719 -1 n -0 0 90 - ULHL LHZ 1998160 718 -1 n -0 0 0 - USP BHE 1993240 522 1993304 n -0 90 90 - USP BHE 1993305 582 1994241 n -0 90 90 - USP BHE 1994242 636 1996091 n -0 90 90 - USP BHE 1991244 426 1992239 n -0 90 90 - USP BHE 1996092 684 -1 n -0 90 90 - USP BHE 1992240 456 1992261 n -0 90 90 - USP BHN 1993305 581 1994241 n -0 0 90 - USP BHN 1991244 425 1992239 n -0 0 90 - USP BHN 1992240 455 1992261 n -0 0 90 - USP BHN 1994242 635 1996091 n -0 0 90 - USP BHN 1996092 683 -1 n -0 0 90 - USP BHN 1993240 521 1993304 n -0 0 90 - USP BHZ 1993240 520 1993304 n -0 0 0 - USP BHZ 1996092 682 -1 n -0 0 0 - USP BHZ 1992240 454 1992261 n -0 0 0 - USP BHZ 1991244 424 1992239 n -0 0 0 - USP BHZ 1994242 634 1996091 n -0 0 0 - USP BHZ 1993305 580 1994241 n -0 0 0 - USP BLE 1993305 585 1994241 n -0 90 90 - USP BLE 1994242 639 1995005 n -0 90 90 - USP BLE 1992261 486 1993239 n -0 90 90 - USP BLE 1993240 525 1993304 n -0 90 90 - USP BLN 1994242 638 1995005 n -0 0 90 - USP BLN 1993305 584 1994241 n -0 0 90 - USP BLN 1993240 524 1993304 n -0 0 90 - USP BLN 1992261 485 1993239 n -0 0 90 - USP BLZ 1993305 583 1994241 n -0 0 0 - USP BLZ 1994242 637 1995005 n -0 0 0 - USP BLZ 1992261 484 1993239 n -0 0 0 - USP BLZ 1993240 523 1993304 n -0 0 0 - USP HHE 1994242 348 1996091 n -0 90 90 - USP HHE 1993305 291 1994241 n -0 90 90 - USP HHE 1993240 231 1993304 n -0 90 90 - USP HHE 1996092 393 -1 n -0 90 90 - USP HHE 1991244 111 1992239 n -0 90 90 - USP HHE 1992240 174 1993239 n -0 90 90 - USP HHN 1993240 230 1993304 n -0 0 90 - USP HHN 1991244 110 1992239 n -0 0 90 - USP HHN 1993305 290 1994241 n -0 0 90 - USP HHN 1996092 392 -1 n -0 0 90 - USP HHN 1992240 173 1993239 n -0 0 90 - USP HHN 1994242 347 1996091 n -0 0 90 - USP HHZ 1992240 172 1993239 n -0 0 0 - USP HHZ 1993240 229 1993304 n -0 0 0 - USP HHZ 1993305 289 1994241 n -0 0 0 - USP HHZ 1991244 109 1992239 n -0 0 0 - USP HHZ 1996092 391 -1 n -0 0 0 - USP HHZ 1994242 346 1996091 n -0 0 0 - USP HLE 1993305 294 1994241 n -0 90 90 - USP HLE 1991244 114 1992239 n -0 90 90 - USP HLE 1994242 345 1995006 n -0 90 90 - USP HLE 1993240 234 1993304 n -0 90 90 - USP HLE 1992240 171 1993239 n -0 90 90 - USP HLN 1994242 344 1995006 n -0 0 90 - USP HLN 1992240 170 1993239 n -0 0 90 - USP HLN 1993305 293 1994241 n -0 0 90 - USP HLN 1991244 113 1992239 n -0 0 90 - USP HLN 1993240 233 1993304 n -0 0 90 - USP HLZ 1994242 343 1995006 n -0 0 0 - USP HLZ 1992240 169 1993239 n -0 0 0 - USP HLZ 1991244 112 1992239 n -0 0 0 - USP HLZ 1993240 232 1993304 n -0 0 0 - USP HLZ 1993305 292 1994241 n -0 0 0 - USP LHE 1998160 717 -1 n -0 90 90 - USP LHN 1998160 716 -1 n -0 0 90 - USP LHZ 1998160 715 -1 n -0 0 0 - VOS BHE 1994205 754 -1 n 0 90 90 - VOS BHN 1994205 755 -1 n 0 0 90 - VOS BHZ 1994205 756 -1 n 0 0 0 - VOS HHE 1994205 757 -1 n 0 90 90 - VOS HHN 1994205 758 -1 n 0 0 90 - VOS HHZ 1994205 759 -1 n 0 0 0 - WQIA BHE 1997271 36 2001365 n -0 90 90 - WQIA BHN 1997271 35 2001365 n -0 0 90 - WQIA BHZ 1997271 34 2001365 n -0 0 0 - WUS BHE 1988305 823 -1 - 0 90 90 WUS BHN 1988305 824 -1 - 0 0 90 WUS BHZ 1988305 825 -1 - 0 0 0 WUS LHE 1988305 817 -1 - 0 90 90 WUS LHN 1988305 818 -1 - 0 0 90 WUS LHZ 1988305 819 -1 - 0 0 0 WUS VHE 1988305 820 -1 - 0 90 90 WUS VHN 1988305 821 -1 - 0 0 90 WUS VHZ 1988305 822 -1 - 0 0 0 XIKR BHE 1999163 45 2001365 n -0 90 90 - XIKR BHN 1999163 44 2001365 n -0 0 90 - XIKR BHZ 1999163 43 2001365 n -0 0 0 - ZRN BHE 1994203 760 -1 n 0 90 90 - ZRN BHN 1994203 761 -1 n 0 0 90 - ZRN BHZ 1994203 762 -1 n 0 0 0 - ZRN HHE 1994203 763 -1 n 0 90 90 - ZRN HHN 1994203 764 -1 n 0 0 90 - ZRN HHZ 1994203 765 -1 n 0 0 0 - ZRNK BHE 1995143 799 -1 n 0 90 90 - ZRNK BHN 1995143 800 -1 n 0 0 90 - ZRNK BHZ 1995143 801 -1 n 0 0 0 -
Total: 825
Selected References
- Martynov, V.G., F.L.Vernon, D.L. Kilb, and S.W. Roecker, 2004, Directional variation in travel-time residuals of teleseismic P-waves in the crust and mantle beneath northern Tien Shan, Bull. Seism. Soc. Am., 94, 650-664
- Martynov, V.G., and F.L. Vernon, 2001, The directional deviations of polarization of teleseismic P waves recorded by KNET in the northern Tien Shan, Fall 2001 AGU Meeting, 813
- Roecker, S.W., X. Yi, and V. Martynov, 2001, Local and regional earthquakes depths in the Tien Shan: evidence for a strong low crust in an active orogen, Fall 2001 AGU Meeting, 1104
- Eakins, J.A., Vernon, F.L., Pavlis, G., Roecker, S., Wallace, T.C. and Martynov, V., 2001, A Central Asian Seismic Bulletin: Utilizing the KNET, Kaznet, and Tien Shan Data Sets, Fall 2001 AGU Meeting, S11B-0571
- Martynov, V.G., F.L. Vernon, and S.W. Roecker, 2000, Azimuthal anisotropy and low velocity structure in the mantle under Kazakh shield and the northern Tien Shan from P wave travel-time data, International Workshop June 7-10, Bishkek, Kyrgyzstan
- Martynov, V.G., F.L. Vernon, R.J. Mellors, and G.L. Pavlis, 1999, High-frequency attenuation in the crust and upper mantle of the northern Tien Shan, Bull. Seism. Soc. Am., 89, 215-238
- Martynov, V.G. and F.L. Vernon, 1999, Azimuthal anisotropy and low velocity structure in the mantle under the northern Tien Shan from P wave travel-time data, Fall 1999 AGU Meeting, 683
URL: http://eqinfo.ucsd.edu/deployments/tien_shan.php [Last updated: 2006-10-26 (299) 22:47:21 UTC]
