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众所周知,地壳的不同地层均按自己特性反射地震波,并按此原理建立了记录和预报地震及勘探有益矿物的各种方法。近几年来,在地质学科内形成了一个有助于研究地球深部构造的独立学科——地震地层学。在此类研究中,计算技术起着特殊作用。电子计算机能够综合全部地震记录并相当准确地确定地壳和上地幔(达80—100公里深度)不同区段的几何形状。在白俄罗斯的普里皮亚特拗陷和在研究巴伦支海—卡拉海大陆架时,均进行了这类研究;后来,电子计算机作的“图像”已部分地由钻探结果所证实。采用地震地层学方法建立了整个西西伯利亚的三维构
As we all know, different layers of the crust reflect seismic waves according to their own characteristics, and according to this principle, various methods for recording and forecasting earthquakes and exploring beneficial minerals are established. In recent years, an independent discipline that contributes to the study of the deep structure of the Earth - the seismic stratigraphy - has been formed within the discipline of geology. In such studies, computing technology plays a special role. The computer can synthesize the complete seismogram and fairly accurately determine the geometry of the different sections of the crust and the upper mantle (up to a depth of 80-100 km). Such studies were conducted during the Pripyat depression in Belarus and during the study of the continental shelf in the Barents Sea-Karaha Sea; later, the “images” made by computerized computers were partly confirmed by drilling results. Seismological stratigraphy was used to establish the three-dimensional structure of the entire West Siberia