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湖相碳酸盐岩研究现状及意义
引用本文:夏青松,田景春,倪新锋.湖相碳酸盐岩研究现状及意义[J].沉积与特提斯地质,2003,23(1):105-112.
作者姓名:夏青松  田景春  倪新锋
作者单位:成都理工大学,沉积地质研究所,四川,成都,610059
摘    要:目前湖相碳酸盐岩是国内外沉积学研究的薄弱环节。本文在众多专家学者历年研究成果的基础上,综述了湖相碳酸盐岩的研究现状,其主要体现在岩石类型、分布及发育特点、相模式、储集层和生油岩几个方面;并阐明了湖相碳酸盐岩的研究具有重要的理论和经济意义。

关 键 词:湖相碳酸盐岩  沉积学  分布  储集层  生油岩  岩石类型
文章编号:1009-3850(2003)01-0105-08
收稿时间:2002/9/16 0:00:00
修稿时间:2002年9月16日

Lacustrine carbonate rocks in China: An overview
XIA Qing-song,TIAN Jing-chun,NI Xin-feng.Lacustrine carbonate rocks in China: An overview[J].Sedimentary Geology and Tethyan Geology,2003,23(1):105-112.
Authors:XIA Qing-song  TIAN Jing-chun  NI Xin-feng
Institution:Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China
Abstract:In spite of great economic significance, very little is known about the lacustrine carbonate rocks both at home and abroad. The present paper, referenced to the previous data, gives an overview of the lacustrine carbonate rocks in China on the basis of rock types, distribution, facies models, reservoir rocks and source rocks. Future researches should focus on the evolution of the lacustrine carbonate rocks during geologic times; physical and chemical conditions for the formation of the lacustrine carbonate rocks in distinctive environments; relationship between the formation of the lacustrine carbonate rocks and transgressions, and that between oil-generating and reservoir capacities and environments in which the lacustrine carbonate rocks were deposited.
Keywords:lacustrine carbonate rock  rock type  facies model  reservoir rock  source rock
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