Title: Seismic Evidence of Strike-Slip Faults in the Middle of Fangzheng Rift and Favorable Exploration Areas
Abstract: Fangzheng rift is a negative tectonic units in the north-central part of Yi-Shu rift.In order to understand the formation mechanism of the basin and the nature of fault system,the new 3D seismic data is used to interpret the structure.The study found that six seismic and geological evidences,for instance,the flower structure and dolphin effect,can prove that strike-slip fault developed.Fangzheng rift is a strike-slip fault related basin.The strike-slip fault's petroleum geological characteristics indicate that the slope-break zone of Deshantun depression is a favorable exploration area.
Publication Year: 2010
Publication Date: 2010-01-01
Language: en
Type: article
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Cited By Count: 5
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