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酒西拗陷下白垩统藻纹层发育环境及形成机制
引用本文:高 波,程克明 樊太亮 涂建琪 熊英. 酒西拗陷下白垩统藻纹层发育环境及形成机制[J]. 西南石油大学学报(自然科学版), 2007, 29(4): 44-48. DOI: 10.3863/j.issn.1000-2634.2007.04.10
作者姓名:高 波  程克明 樊太亮 涂建琪 熊英
作者单位:1.中国地质大学,北京 100083;2.中国石化石油勘探开发研究院;3.中国石油勘探开发研究院
摘    要:酒西拗陷下白垩统纹层状泥质白云岩和白云质泥岩中藻纹层十分发育,主要由浮游藻类及其降解产物组成。藻纹层发育状况在很大程度上决定了该区下白垩统烃源岩生烃能力的大小,这也是烃源岩呈现出较强非均质性的一个重要原因。对酒西拗陷下白垩统藻纹层的发育条件及保存环境进行了研究,并对其形成机制进行了探讨。研究结果表明,早白垩世,酒西拗陷断陷湖盆水体广泛,适宜的温度、盐度等介质条件有利于藻类的大量繁殖,而水体分层的强还原环境对有机质的保存较为有利。湖泊水体的季节性更替及其引起的水体分层是该区藻纹层形成的重要原因。

关 键 词:烃源岩  藻纹层  发育条件  形成机制  酒西拗陷  
收稿时间:2006-08-31

DEVELOPMENT ENVIRONMENT AND FORMATION MECHANISM OF ALGAE LAMINAE IN LOWER CRETACEOUS IN JIUXI DEPRESSION
GAO Bo,CHENG Ke-ming FAN Tai-liang et al. DEVELOPMENT ENVIRONMENT AND FORMATION MECHANISM OF ALGAE LAMINAE IN LOWER CRETACEOUS IN JIUXI DEPRESSION[J]. Journal of Southwest Petroleum University(Seience & Technology Edition), 2007, 29(4): 44-48. DOI: 10.3863/j.issn.1000-2634.2007.04.10
Authors:GAO Bo  CHENG Ke-ming FAN Tai-liang et al
Affiliation:China University of Geosciences, Beijing 100083, China
Abstract:The organic matter laminae composed of algae and its decomposition products is very abundant in argillaceous dolomite and dolomitic mudstone of the Lower Cretaceous in the Jiuxi Depression. The development of algae laminae greatly enhances the hydrocarbon generating ability of source rocks in the research area and is one of important reasons why the source rocks are heterogeneous. In this paper, development and reservation environment and formation mechanism of algae laminae in the Cretaceous source rocks are discussed, and the formation mechanism of algae laminae is probed. The research results show that in the early Cretaceous, the capaciousness of lake water, moderate temperature and salinity are favorite for the algae blooming. However, the strong reductive environment made by layering of lake water is greatly of advantage to reservation of organic matters. Seasonal change of lake water and its layering are the important reasons of the formation of algae laminae.
Keywords:source rocks  algae laminae  development condition  formation mechanism  Jiuxi depression  
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