Testing Event Discrimination over Broad Regions using the Historical Borovoye Observatory Explosion Dataset
We test the performance of high-frequency regional P/S discriminants to differentiate between earthquakes and explosions at test sites and over broad regions using a historical dataset of explosions recorded at the Borovoye Observatory in Kazakhstan. We compare these explosions to modern recordings...
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Veröffentlicht in: | Pure and applied geophysics 2014-03, Vol.171 (3-5), p.523-535 |
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creator | Pasyanos, Michael E. Ford, Sean R. Walter, William R. |
description | We test the performance of high-frequency regional P/S discriminants to differentiate between earthquakes and explosions at test sites and over broad regions using a historical dataset of explosions recorded at the Borovoye Observatory in Kazakhstan. We compare these explosions to modern recordings of earthquakes at the same location. We then evaluate the separation of the two types of events using the raw measurements and those where the amplitudes are corrected for 1-D and 2-D attenuation structure. We find that high-frequency P/S amplitudes can reliably identify earthquakes and explosions, and that the discriminant is applicable over broad regions as long as propagation effects are properly accounted for. Lateral attenuation corrections provide the largest improvement in the 2–4 Hz band, the use of which may successfully enable the identification of smaller, distant events that have lower signal-to-noise at higher frequencies. We also find variations in P/S ratios among the three main nuclear testing locations within the Semipalatinsk Test Site which, due to their nearly identical paths to BRVK, must be a function of differing geology and emplacement conditions. |
doi_str_mv | 10.1007/s00024-012-0591-4 |
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Geophys</addtitle><description>We test the performance of high-frequency regional P/S discriminants to differentiate between earthquakes and explosions at test sites and over broad regions using a historical dataset of explosions recorded at the Borovoye Observatory in Kazakhstan. We compare these explosions to modern recordings of earthquakes at the same location. We then evaluate the separation of the two types of events using the raw measurements and those where the amplitudes are corrected for 1-D and 2-D attenuation structure. We find that high-frequency P/S amplitudes can reliably identify earthquakes and explosions, and that the discriminant is applicable over broad regions as long as propagation effects are properly accounted for. Lateral attenuation corrections provide the largest improvement in the 2–4 Hz band, the use of which may successfully enable the identification of smaller, distant events that have lower signal-to-noise at higher frequencies. We also find variations in P/S ratios among the three main nuclear testing locations within the Semipalatinsk Test Site which, due to their nearly identical paths to BRVK, must be a function of differing geology and emplacement conditions.</description><subject>Amplitudes</subject><subject>Attenuation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Environmental monitoring</subject><subject>Explosions</subject><subject>Geophysics/Geodesy</subject><subject>Nuclear accidents & safety</subject><subject>Nuclear weapons</subject><subject>Observatories</subject><subject>Position (location)</subject><subject>Recording</subject><subject>Seismic activity</subject><subject>Seismic phenomena</subject><issn>0033-4553</issn><issn>1420-9136</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kE1LxDAQhoMouK7-AG8BL16qk6RfObofusLCguw9pO107dpt1qQt7r83pR5E8DQwPO_LzEPILYMHBpA8OgDgYQCMBxBJFoRnZMJCDoFkIj4nEwAhgjCKxCW5cm4PwJIkkhPysUXXVs2OLntsWrqoXG6rQ9XotjINNT1aOrNGF_QNd37jaOcGun1Huqpca2yV65rOjDW9OSHdZA5tr_3-RJdfx9q4oWahW-2wvSYXpa4d3vzMKdk-L7fzVbDevLzOn9aBFglvgzjVUsfIMxEjyyJI8khmpUwZ8DLGMuMMozJPcx1DKFMZap1xmRdlIbQshBBTcj_WHq357Px76uC_wrrWDZrOKRZxkN4EB4_e_UH3prONP85TECZMcC49xUYqt8Y5i6U6ekfanhQDNdhXo33l7avBvgp9ho8Z59lmh_ZX87-hb3NYiNo</recordid><startdate>20140301</startdate><enddate>20140301</enddate><creator>Pasyanos, Michael E.</creator><creator>Ford, Sean R.</creator><creator>Walter, William R.</creator><general>Springer Basel</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20140301</creationdate><title>Testing Event Discrimination over Broad Regions using the Historical Borovoye Observatory Explosion Dataset</title><author>Pasyanos, Michael E. ; 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Geophys</stitle><date>2014-03-01</date><risdate>2014</risdate><volume>171</volume><issue>3-5</issue><spage>523</spage><epage>535</epage><pages>523-535</pages><issn>0033-4553</issn><eissn>1420-9136</eissn><abstract>We test the performance of high-frequency regional P/S discriminants to differentiate between earthquakes and explosions at test sites and over broad regions using a historical dataset of explosions recorded at the Borovoye Observatory in Kazakhstan. We compare these explosions to modern recordings of earthquakes at the same location. We then evaluate the separation of the two types of events using the raw measurements and those where the amplitudes are corrected for 1-D and 2-D attenuation structure. We find that high-frequency P/S amplitudes can reliably identify earthquakes and explosions, and that the discriminant is applicable over broad regions as long as propagation effects are properly accounted for. Lateral attenuation corrections provide the largest improvement in the 2–4 Hz band, the use of which may successfully enable the identification of smaller, distant events that have lower signal-to-noise at higher frequencies. We also find variations in P/S ratios among the three main nuclear testing locations within the Semipalatinsk Test Site which, due to their nearly identical paths to BRVK, must be a function of differing geology and emplacement conditions.</abstract><cop>Basel</cop><pub>Springer Basel</pub><doi>10.1007/s00024-012-0591-4</doi><tpages>13</tpages></addata></record> |
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subjects | Amplitudes Attenuation Earth and Environmental Science Earth Sciences Earthquakes Environmental monitoring Explosions Geophysics/Geodesy Nuclear accidents & safety Nuclear weapons Observatories Position (location) Recording Seismic activity Seismic phenomena |
title | Testing Event Discrimination over Broad Regions using the Historical Borovoye Observatory Explosion Dataset |
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