石油与天然气地质 ›› 1995, Vol. 16 ›› Issue (4): 374-378.doi: 10.11743/ogg19950413

• 论文 • 上一篇    下一篇

松辽南部早白垩世断陷期沉积相与成岩相

陈振林, 王果寿, 王筠, 卿崇文   

  1. 湖北荆沙地质矿产部石油地质综合大队, 湖北荆沙, 434100
  • 收稿日期:1994-07-22 修回日期:1995-06-10 出版日期:1995-12-25 发布日期:2012-01-16
  • 基金资助:

    国家“八五”攻关课题(85-102-09-01)

SEDIMENTAL AND DIAGENETIC FACIES OF EARLY CRETACEOUS FAULT-SUBSIDENCE STAGE IN SOUTH SONGLIAO

Chen Zhenlin, Wang Guoshou, Wang Yu, Qing Chongwen   

  1. Comprehensive Reserch Institute of Petroleum Geology, MGMR, Jingsha, Hubei
  • Received:1994-07-22 Revised:1995-06-10 Online:1995-12-25 Published:2012-01-16

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摘要：

松辽南部早白垩世断陷期地层地震相分析显示,该时期冲积扇、三角洲、水下扇及扇三角洲沉积体系十分发育,是深部油(气)聚集的有利场所。登娄库组可分出:浅埋弱压实成岩相、晚表生溶蚀成岩相、深埋溶蚀成岩相、深埋压溶成岩相,以前二者为油气聚集的有利成岩相。

关键词: 断陷期, 沉积相, 地震相, 成岩作用, 成岩相

Abstract:

The seismic analysis of the Early Cretaceous fault-subsidence stage in South Songliao Basin suggests that the depositional system including alluvial fan-delta, subaqueous fan, delta and fan-delta developed well, and they are favourable for oil and gas accumulation. The Denglouku Formation in the study area could be divided into shallow buried-weak compacted diagenetic factes,supergene dissolution diagenetic factes, deep-buried dissolution diagenetic factes and deep-buried compaction-dissolution diagenetic factes. The first two kinds are favourble factes for hydrocarbon accumulation.