扬子地块西北缘后龙门山南华纪-早古生代沉积地层特征及其形成环境  

Characteristics of Sedimentary Strata and Their Forming Environments of Nanhuan Period-Early Paleozoic of Back-Longmenshan in the Northwest Margin of Yangtze Block

作　　者：李佐臣[1,2] 裴先治[1,2] 刘战庆[2] 李瑞保[1,2] 丁仨平 张晓飞[2] 陈国超[2] 刘智刚[2] 陈有 王学良[2] 

机构地区：[1]长安大学西部矿产资源与地质工程教育部重点实验室,陕西西安710054 [2]长安大学地球科学与资源学院,陕西西安710054

出　　处：《地球科学与环境学报》2011年第2期117-124,共8页Journal of Earth Sciences and Environment

基　　金：国家自然科学基金项目(40972136;40572121;40234041);中央高校基本科研业务费专项资金项目(CHD2009JC046;CHD2009JC053;CHD2009JC070);中国石油化工股份有限公司海相前瞻性研究项目(YPH08006)

摘　　要：通过对扬子地块西北缘后龙门山构造带南华纪—早古生代沉积地层的分析研究,综合运用岩石学、沉积特征分析的手段,结合与前龙门山构造带、碧口地块、米仓山构造带和汉南地块的沉积特征对比,探讨后龙门山构造带南华纪—早古生代的沉积环境,查明其形成环境。结果表明:在南华纪—早古生代后龙门山构造带沉积环境可分为南华纪—震旦纪裂解-稳定沉积和早古生代伸展裂陷沉积两个阶段,其中在早古生代伸展裂陷阶段后龙门山构造带经历了裂解→抬升→局部裂解→抬升→裂解的反复过程,最终形成了志留系茂县群裂陷槽沉积,主要沉积了一套代表伸展裂陷环境的沉积岩系,并有少量的陆内火山岩系。研究结果进一步证实,龙门山构造带在南华纪—早古生代总体是一个陆内裂谷带,不发育与古缝合线相关的构造混杂岩和蛇绿混杂岩带,是在陆内裂谷的基础上于印支期—燕山期形成的陆内造山带。Through the research on sedimentary strata of Nanhuan Period-Early Paleozoic of Back-Longmenshan tectonic belt in the northwest margin of Yangtze Block with the methods of petrology and sedimentary strata,the sedimentary and forming environments of Nanhuan Period-Early Paleozoic of Back-Longmenshan tectonic belt were discussed based on the contrast of sedimentary characteristics of Fore-Longmenshan tectonic belt,Bikou Block,Micangshan tectonic belt and Hannan Block.The results indicated that the sedimentary environments of Nanhuan Period-Early Paleozoic of Back-Longmenshan tectonic belt could be divided into two stages,including the division-stable stage of Nanhuan-Sinian Period and the extension and division-collapse stage of Early Paleozoic;Back-Longmenshan tectonic belt had the repetitive process of divergence→lifting→partial divergence→lifting→divergence during the extension and division-collapse stage of Early Paleozoic;aulacogen sedimentary in Maoxian Group of Silurian System,which represented the extension and division-collapse environment,was eventually formed,and there was a little intra-continental volcanic rocks.The results further confirmed that Back-Longmenshan tectonic belt in general was an intra-continental rift belt during Nanhua Period-Early Paleozoic and an intra-continental orogenic belt based on the intra-continental aulacogen in Indosinian-Yanshanian Period,and did not develop tectonic and ophiolitic melange belts related with the ancient suture.

关 键 词：扬子地块西北缘 后龙门山构造带 南华纪—早古生代 沉积环境 裂陷槽 

分 类 号：P54[天文地球—构造地质学] P53[天文地球—地质学]