摘要
同沉积断层是地层沉积与断层活动共同作用形成的一种构造,其对油气的生成、运移、聚集、储集等有着重要作用。本文就同沉积断层的几何形态及逆牵引构造的特征和形成机理做了重点分析。
Synsedimentary fault is formed by the common faults and strata sedimentary activity of a kind of structure, the oil and gas generation, migration, accumulation and reservoir plays an important role. In this paper, the synsedimentary fault geometry and inverse traction structure characteristics and forming mechanism of key analysis.
出处
《世界有色金属》
2017年第11期278-279,共2页
World Nonferrous Metals
关键词
同沉积断层
逆牵引构造
形成机理
syndepositional fault
reversed drag structure
formation mechanism
