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湖北京山大冶组深水碳酸盐岩沉积特征及沉积相
引用本文:胡明毅 王宝清. 湖北京山大冶组深水碳酸盐岩沉积特征及沉积相[J]. 石油天然气学报, 1994, 16(2): 33-37
作者姓名:胡明毅 王宝清
作者单位:江汉石油学院石油地质系
基金项目:中国石油天然气总公司"八五"攻关课题
摘    要:湖北京山地区下三叠统大冶组主要为一套深水碳酸盐岩,它以深水源泥晶灰岩沉积为主,夹有多种不同成因类型的异地沉积。详细论述了该区大冶组深水沉积的成因类型及其沉积特征,划分了沉积相带,并对该区的古地地理格局进行了讨论。

关 键 词:沉积相 碳酸盐岩 早三叠世

Depositional Characteristics of the Deep - water Carbonate Rocks in Daye Formation (Lower Triassic) from Jingshan, Hubei Province
Hu Mingyi,Wang Baoqing,Hu Aimei,Chen Jianming. Depositional Characteristics of the Deep - water Carbonate Rocks in Daye Formation (Lower Triassic) from Jingshan, Hubei Province[J]. Journal of Oil and Gas Technology, 1994, 16(2): 33-37
Authors:Hu Mingyi  Wang Baoqing  Hu Aimei  Chen Jianming
Abstract:Daye formation (lower Triassic) in Jingshan, Hubei province is mainlycomposed of deep - water autochthonous deposits with various deep - water allochthonousdeposits such as high - density turbidity, debris flow and contour current deposits. Thetypes and depositional characteristics of deep - water carbonate deposits are discussed indetail. and the sedimentary factes are analyzed. Furthermore, the lithofaciespaleogeographic map in studying aren for the stage is given.
Keywords:sedimentary facies   abysmal facies   carbonate rocks   Early Triassic Epoch   (Hubei province)
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