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| 惠民凹陷沙河街组一段白云岩特征及其成因分析 | |
| 引用本文： | 孙钰,钟建华,袁向春.惠民凹陷沙河街组一段白云岩特征及其成因分析[J].沉积与特提斯地质,2007,27(3):78-84. |
| 作者姓名： | 孙钰 钟建华 袁向春 |
| 作者单位： | 1. 中国石化石油勘探开发研究院,北京,100083;中国地质大学,北京,100083 2. 中国石油大学,地球资源与信息学院,山东,东营,257061 3. 中国石化石油勘探开发研究院,北京,100083 |
| 摘 要： | 惠民凹陷沙河街组一段发育大量的湖相碳酸盐岩,综合岩心、录井、地化及微观资料分析碳酸盐岩特征。碳酸盐岩中发育大量的白云岩,其常见岩石类型包括生物碎屑云岩、灰质藻云岩、砾屑云岩、鲕粒云岩、泥(粉)晶云岩五大类;且白云岩在深湖、半深湖、浅湖、滩坝环境均有发育,垂向上与油页岩、泥岩、生物灰岩及火山岩共生。研究表明,沙一段白云岩为次生交代的产物,且海侵作用、古气候条件和火山活动均为湖相白云岩的形成创造了条件。 |
| 关 键 词： | 白云岩 成因 沙河街组 惠民凹陷 |
| 文章编号： | 1009-3850（2007）03-0078-07 |
| 收稿时间： | 2006-12-05 |
| 修稿时间： | 2006年12月5日 |
Genesis of the dolostones from the first member of the Shahejie Formation in the Huimin depression, Shandong |
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| SUN Yu,ZHONG Jian-hu,YUAN Xiang-chun.Genesis of the dolostones from the first member of the Shahejie Formation in the Huimin depression, Shandong[J].Sedimentary Geology and Tethyan Geology,2007,27(3):78-84. | |
| Authors: | SUN Yu ZHONG Jian-hu YUAN Xiang-chun |
| Institution: | 1. Research Institute of Petroleum Exploration and Development, SINOPEC, Beijing 100083, China; 2. China University of Geosciences, Beijing 100083, China ; 3. Faculty of Earth Resources and Information, China University of Petroleum, Dongying 257061, Shandong, China |
| Abstract: | There widely occur in the Huimin depression the dolostones including bioclastic dolostone,lime algal dolostone,dolorudite,oolitic dolostone and micritic dolostone developed in the abyssal lake,bathyal lake,shallow lake,and shoal and bar environments.Vertically,these dolostones are associated with oil shale,mudstone,bioclastic limestone and volcanic rocks,and interpreted as the secondary replacement products.The transgression,palaeoclimate and volcanism have exerted an important effect on the formation of the lacustrine dolostones. |
| Keywords: | dolostone genesis Shahejie Formation Huimin depression |
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