石油与天然气地质 ›› 1990, Vol. 11 ›› Issue (3): 320-333.doi: 10.11743/ogg19900315

• 论文 • 上一篇    下一篇

下扬子复合地体与含油气性特征

龚与觐   

  1. 地质矿产部华东石油地质局
  • 收稿日期:1989-06-24 修回日期:1989-12-24 出版日期:1990-09-25 发布日期:2012-01-16

COMPOSITE TERRANE AND ITS HYDROCARBON POTENTIAL IN LOWER YANGTZE REGION

Gong Yujin   

  1. Huadong Bureau of Petroleum Geology, Ministry of Geology and Mineral Resources
  • Received:1989-06-24 Revised:1989-12-24 Online:1990-09-25 Published:2012-01-16

PDF (PC)

552

被引次数

4

摘要：

下扬子区基底性质、盖层岩相、构造特征,以及岩浆活动等,存在明显的南北分异。造成这些差异的原因,是存在南(钱塘)、北(扬子)两个地体,经长期的构造演化,至三叠纪末期才拼贴成一个统一的复合地体的结果。钱塘地体下古生界和扬子地体上古生界(含三叠系)是烃类生成、聚集的有利领域;应以钱塘地体作为油气勘探的重点。

关键词: 下扬子区, 复合地体, 钱塘地体, 扬子地体, 构造演化, 含油气盆地, 油气资源评价, 古生界

Abstract:

The basement nature,the cover facies,the structural feature and magmatic activity in the lower Yangtze Region have presented obvious differentiae in the north and south parts of the region.The reason caused these differences is the existence of south (the Qiantang) and north (the Yangtze) terranes.These two terranes,under went long tectonicevolution,were connected as a unified composite terrane in the end of the Triassic.The Qiantang Terrane is the primary place for hydrocarbon generation and accumulation from Lower Paleozoic;the Yangtze Terrane is the most favourable place for thatfrom Upper Paleozoic (including the Middle and Lower Triassic).The former will be themain target for oil and gas exploration.