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塔里木西部石炭—二叠纪沉积体系特征
引用本文:德勒达尔.塔里木西部石炭—二叠纪沉积体系特征[J].新疆地质,1996(4).
作者姓名:德勒达尔
作者单位:新疆石油学院勘探系
摘    要:对塔里木西部地区30余条剖面及钻井资料的全面系统分析研究,结合地震资料,认为石炭-二叠纪为一个完整的海进至海退旋回。在海进初期和海退末期为碳酸盐岩和碎屑岩混积时期,用"混积陆棚"的概念,将石炭-二叠系划分为下石炭统(个别地区的下二叠统下部)混积陆棚沉积体系;上石炭统至下二叠统下部为碳酸盐岩台地沉积体系;下二叠统上部至上二叠统为陆源碎屑沉积体系。

关 键 词:塔里木西部,石炭-二叠纪,沉积体系,混积陆硼,碳酸盐岩台地

SEDIMENTARY SYSTEM OF CARBONIFEROUS-PERMIAN OF WESTERN TARIM
Deledaer.SEDIMENTARY SYSTEM OF CARBONIFEROUS-PERMIAN OF WESTERN TARIM[J].Xinjiang Geology,1996(4).
Authors:Deledaer
Abstract:Coupled with seismic data, a systematic research of over 3o sections add drilling data show that Carboniferous-Permian is a complete cycle from progression to regression. During the eatly st age of progression and late stage of regression carbonates and elastics occured in a melapged accumulation.Applying the concept of "melanged accumulation shelf" the Carboniferous-Persian can be subdivided into Lower Carboniferous melanged accumulation shelf system, Upper Carboniferous-lower part of Lower Permian carbonates platform sedimentary system, and upper part of Lower Permian-Upper Permian terrigenous clastic,sedimentary systems.
Keywords:western Tarim Carboniferous-Permian sedimentary system melanged accumulation shelf canbonates platform  
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