CRUSTAL STRUCTURE IN SEISMIC AND ASEISMIC REGIONS BASED ON GEOTRAVERSE DATA: BAZALT, RUBIN, KVARTS, AND ARMASH-AKHALTSIKHE GEOTRAVERSES
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dc.contributor.author | Popova O.G. | |
dc.contributor.author | Konovalov Y.F. | |
dc.contributor.author | Solodilov L.N. | |
dc.contributor.author | Popov M.G. | |
dc.date.accessioned | 2021-01-14T07:58:12Z | |
dc.date.available | 2021-01-14T07:58:12Z | |
dc.date.issued | 1999 | |
dc.identifier | https://elibrary.ru/item.asp?id=20939929 | |
dc.identifier.citation | Volcanology & Seismology, 1999, 20, 4, 563-596 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/22973 | |
dc.description.abstract | An analysis of deep crustal structure and seismicity was performed along four traverses (Bazalt, Rubin, Kvarts, and Armash-Akhaltsikhe), which cut across seismic areas, to detect differences in crustal structure between geologic features exhibiting differing degrees of seismic activity. The original information included estimates of V(P), V(S), γ = V(P)/V(S), and the geometry of crustal blocks derived from interpretations of materials furnished by deep explosion seismic and earthquake-generated exchange-wave profiles processed at the GEON Center. The software of the GEO data processing system was used [3], [4]. A set of patterns was found to recognize areas of possible damaging earthquakes; this can be the starting point for further studies in these areas, for deployment of local seismographic networks, and for geophysical monitoring for the purpose of short-term and intermediate-term earthquake prediction. | |
dc.title | CRUSTAL STRUCTURE IN SEISMIC AND ASEISMIC REGIONS BASED ON GEOTRAVERSE DATA: BAZALT, RUBIN, KVARTS, AND ARMASH-AKHALTSIKHE GEOTRAVERSES | |
dc.type | Статья |
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