石油与天然气地质 ›› 1986, Vol. 7 ›› Issue (3): 224-235.doi: 10.11743/ogg19860304

• 论文 • 上一篇    下一篇

中扬子沉积盆地构造及其形成与演化

张文荣, 戴少武   

  1. 江汉石油管理局勘探开发研究院
  • 收稿日期:1985-12-10 修回日期:1986-03-08 出版日期:1986-09-25 发布日期:2012-01-16

GEOLOGICAL TECTONICS OF CENTRAL YANGZI BASIN AND THEIR FORMATION AND EVOLUTION

Zhang Wenrong, Dai Shaowu   

  1. Research Institute of Petroleum Exploration and Development, Jianghan Petroleum Administration
  • Received:1985-12-10 Revised:1986-03-08 Online:1986-09-25 Published:2012-01-16

摘要:

本区在中条-武陵运动形成的基底上,先后形成震旦纪—中三叠世广海盆地,晚三叠世—侏罗纪内陆大型湖沼含煤沉积盆地,江汉白垩—第三纪多旋回盐湖沉积盆地。现今主要构造单元包括中部的江汉盆地,东北、东南缘的逆冲构造带,西部的重力滑覆褶断带。本区先天性成油气条件优越,但不少地区的海相沉积后期改造剧烈,然上述三构造单元仍具有一定的含油气远景。

Abstract:

Central Yangzi Basin belongs to the central part of Yangzi Paraplatform.Its basement was formed by Zhongtiao-Wuling Orogenies.The basin experienced multy-stage and multy type tectogenesis dominated by compressive tectonic en-vironment,thus the open-sea basin in the Sinian-Middle Triassic,huge coal-bearing lacustrine basin of the intercont inent in the Late Triassic to Jurassic andmultycycle basin of the brine lake in the Cretaceous to Tertiary were formed before and after.The main tectonic units of the present time include Jianghan Basin in the central part of the platform,overthrust tectonic belts in the north-eastern and southeastern margin and gravity-glide faults in the west part ofthe region.The basin has congenitally favourable conditions for hydrocarbon generation due to its great thickness of sedimental covers and multyple source-reservoir rock as semblages.The above mentioned three tectonic units are still prospectivefor oil and gas exploration though marine sediments there were seriously damaged by Yanshan Orogeny.The authors suggest that we have to take the compre hensiveresearch with the purpose of breaking through the Paleozoic-Mesozoic oil and gad on the basis of regional geophysical prospecting and parameter-well drilling.