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克参1井白垩系划分对比的初步探讨
Primary Discussion on the Cretaceous Division and Correlation of Well KC1
【摘要】 本文从古生物特征、岩性特征及区域地层分布规律入手,对克参1井白垩系划分对比进行了详细探讨,并解释了白垩系厚度巨大及未钻遇侏罗系的原因。指出:井探2700~6150米地层归属白垩系,可划分为三个组,本井未钻遇侏罗系。
【Abstract】 Starting with the analyses of paleontological, lithological characters and strata regional distri-bution, this paper pays more attention to the division and correlation of Cretaceous System andgives a explanation why cretaceous is enormous in thickness and Jurassic has not been encounteredby drilling. A Suggestion is made here that the sediments at depths 2700~6150m belong to Creta-ceous System which can be divided into three Formations and no Jurassic sediments has been en-countered in this well.
【关键词】 塔里木盆地;
克参1井;
白垩系;
划分;
对比;
【Key words】 Tarim basin; Well Kc1; Cretaceous; Division; Correlation;
【Key words】 Tarim basin; Well Kc1; Cretaceous; Division; Correlation;
- 【文献出处】 新疆石油学院学报 ,JOURNAL OF XINJIANG PETROLEDM INSTITUTE , 编辑部邮箱 ,1998年01期
- 【分类号】P618.13
- 【下载频次】39