四川盆地东部上三叠统须家河组地层划分与对比——以卧新双地区为例

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英文篇名：STRATIGRAPHIC SUBDIVISION AND CORRELATION OF THE EARLY TRIASSIC XUJIAHE FORMATION,EAST SICHUAN BASIN:A CASE STUDY OF THE WOXINSHUANG AREA 作者：王昌勇 ; 郑荣才 ; 李爽 ; 李世临 ; 李国辉 ; 王小娟 ; 戴朝成 英文作者：WANG Chang-yong;ZHENG Rong-cai;LI Shuang;LI Shi-lin;LI Guo-hui;WANG Xiao-juan;DAI Zhao-cheng;Institute of Sedimentary Geology of Chengdu University of Technology;Chongqing Gas Field,PetroChina Southwest Oil and Gas Field Company;Research Institute of Exploration and Development,PetroChina Southwest Oil and Gas Field Company; 关键词：岩石地层 ; 地层对比 ; 不整合 ; 安县运动 ; 须家河组 ; 香溪群 ; 三叠系 ; 川东地区 英文关键词：lithostratigraphy;;stratigraphic correlation;;unconformity;;Anxian Movement;;Xujiahe Formation;;Xiangxi Group;;Triassic;;Sichuan Basin 中文刊名：DCXZ 英文刊名：Journal of Stratigraphy 机构：成都理工大学沉积地质研究院;中国石油西南油气田分公司重庆气矿;中国石油西南油气田分公司勘探开发研究院; 出版日期：2017-01-15 出版单位：地层学杂志 年：2017 期：v.41 基金：国家科技重大专项“四川盆地岩性油气藏富集规律与目标评价(编号:2011ZX05001-005)”;; 国家自然科学青年基金“川中地区须家河组砂岩中自生绿泥石成分演化及其地质意义(编号:41402085)”部分研究成果 语种：中文; 页：DCXZ201701012 页数：9 CN：01 ISSN：32-1187/P 分类号：96-104

摘要

主要根据野外露头资料、钻井岩芯和测井资料,对川东地区须家河组岩石特征、剖面结构和沉积环境进行了详细研究,首次发现了舌形贝化石,确定川东须家河组底部发育海相沉积,并在须家河组内部发现砾岩层和角度不整合面,确定安县运动对川东须家河组沉积有很大影响。从须家河组沉积前四川盆地古地貌特征、须家河组沉积初期古地理面貌、沉积构造、古生物特征及关键性层序界面等多个方面论证了川东地区发育须一段沉积,同时根据须家河组顶、底及内部不整合3个关键界面对川东须家河组进行了层序地层划分和区域地层对比,认为川东地区须家河组发育须一段~须六段6个相对完整的岩性段:须一段主要为一套有障壁海岸的瀉湖-潮坪或海湾沉积,须二段~须六段主要为辫状河三角洲沉积,其中须三段及须五段仍以细、中砂岩为主,这一特征有别于广安及龙岗等靠近盆地的其他区域,但正好反映了陆相三角洲沉积体系从盆地边缘到盆地中央砂岩逐渐减少的一般规律。
        Based on outcrop,drilling core,and well log data,the stratigraphy and sedimentary environments of the Early Triassic Xujiahe Formation in eastern Sichuan Province were analyzed.We report for the first time lingulid fossils from the Xujiahe Formation in eastern Sichuan Basin,suggesting a marine sedimentary facies for this stratigraphic unit.We also report a gravel layer and an angular unconformity within the Xujiahe Formation,suggesting that the Anxian Movement may have had an impact on the sedimentation of the Xujiahe Formation.Based on paleogeomorphic analysis,sedimentary structures,and paleontological data,it is demonstrated that the First Member of the Xujiahe Formation is well developed in eastern Sichuan Basin.Three unconformities,at the base and top and within the Xujiahe Formation,have been recognized.The Xujiahe Formation in eastern Sichuan can be divided into six members(First to Sixth Member).The First Member of the Xujiahe Formation is characterized by lagoonal-tidal flat coastal barrier or gulf deposits,and Seconde to Sixth Member of the Xujiahe Formation consist mainly of braided river delta deposits,with Third Member and Fifth Member consisting mainly of fine-medium sandstones.These sedimentary environments are different from those of the Xujiahe Formation in other areas such as Guang'an and Longgang which were near the center of the basin and are characterized by finer-grained sediments and fewer sandstone beds.

引文

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