石油与天然气地质 ›› 2002, Vol. 23 ›› Issue (1): 99-102.doi: 10.11743/ogg20020122

• 油气空间 • 上一篇    下一篇

塔河地区石炭系沉积特征

郭齐军1, 赵省民2   

  1. 1. 中国石油化工股份公司油田事业部, 北京, 100029;
    2. 中国地质科学院矿床地质所, 北京, 100010
  • 收稿日期:2001-11-22 出版日期:2002-03-25 发布日期:2012-01-16

DEPOSITIONAL CHARACTERISTICS OF CARBONIFEROUS IN TAHE REGION

Guo Qijun1, Zhao Xingmin2   

  1. 1. Oilfield E & D Department, SINOPEC, Beijing;
    2. Research Institute of Deposit Geology, Chines Academy of Geological Sciences, Beijing
  • Received:2001-11-22 Online:2002-03-25 Published:2012-01-16

PDF (PC)

653

被引次数

34

摘要：

塔河地区石炭系仅发育下石炭统巴楚组和卡拉沙依组。经研究,石炭系中共发育块状砂质砾岩相、板块交错层理含砾砂岩相、槽状交错层理含砾砂岩相、板状交错层理砂岩相等 11种沉积微相。石炭系中共识别出 4大沉积体系 :辫状河三角洲体系、三角洲体系、泻湖-潮坪体系和碳酸岩台地体系。其中,辫状河三角洲体系最为发育,是石炭系的主要组成部分;碳酸岩台地体系发育最为局限,仅在巴楚组底部见到。

关键词: 微相, 沉积体系, 石炭系, 塔河地区

Abstract:

The Lower Carboniferous Bachu Formation and Karashayi Formation developed in Tahe Region could be divided into massive sandy conglomerate facies,platy cross-bedded conglomeratic sandstone facies,trough cross-bedded conglomeratic sandstone facies,platy cross-bedded sandstone facies and 4 depositional systems such as braided river delta system,delta system,lagoon-flat system and carbonate platform system.The braided river delta system developed well in the region,and plays the main part of the Carboniferous System;carbonate platform could only be found on the bottom of the Bachu Formation.

Key words: microfacies, depositional system, Carboniferous System, Tahe Region

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