川西龙门山褶皱冲断带分带性变形特征

英文篇名：Deformation and Zonation of the Longmenshan Fold and Thrust Zone in the Western Sichuan Basin
中文刊名：地质学报
英文刊名：Acta Geologica Sinica
作者：金文正 ; 汤良杰 ; 杨克明 ; 万桂梅 ; 吕志洲 ; 余一欣
英文作者：JIN Wenzheng1 ; 2 ; 3) ; TANG Liangjie1 ; 2 ; 3) ; YANG Keming4) ; WAN Guimei1 ; 2 ; 3) ; L Zhizhou4) ; YU Yixin1 ; 2 ; 3)1) State key laboratory for Petroleum Resource and Prospecting ; Beijing ; 1022492) Key Laboratory for Hydrocarbon Accumulation Mechanism ; China University of Petroleum ; Ministry of Education ; Beijing ; 1022493) Basin and Reservoir Research Centre ; China University of Petroleum ; Beijing ; 1022494) Southwest Division Company ; SINOPEC ; Chengdu ; 610081
中文关键词：分带性变形 ; 松潘-甘孜构造带 ; 基底卷入冲断带 ; 前陆坳陷带 ; 龙门山褶皱冲断带
英文关键词：zonation deformation ; Songpan-Graze tectonic belt ; the basement involution fold and thrust belt ; the foreland depression belt ; Longmen Mountain
出版日期：2007-08-15
机构：油气资源与探测国家重点实验室,油气资源与探测国家重点实验室,中国石油化工股份有限公司西南分公司,油气资源与探测国家重点实验室,中国石油化工股份有限公司西南分公司,油气资源与探测国家重点实验室北京,102249 石油天然气成藏机理教育部重点实验室,中国石油大学,北京,102249 中国石油大学盆地与油藏研究中心,北京,102249,北京,102249 石油天然气成藏机理教育部重点实验室,中国石油大学,北京,102249 中国石油大学盆地与油藏研究中心,北京,102249,成都,610081,北京,102249 石油天然气成藏机理教育部重点实验室,中国石油大学,北京,102249 中国石油大学盆地与油藏研究中心,北京,102249,成都,610081,北京,102249 石油天然气成藏机理教育部重点实验室,中国石油大学,北京,102249 中国石油大学盆地与油藏研究中心,北京,102249
年：2007
期：08
出版单位：地质学报

摘要

通过野外地质考察和地震资料解释,将龙门山褶皱冲断带划分为5个构造带,即青川-茂汶断裂以西为松潘-甘孜构造带,青川-茂汶断裂与北川-映秀断裂之间为韧性变形带,北川-映秀断裂与马角坝-通济场-双石断裂之间为基底卷入冲断带,马角坝-通济场-双石断裂与广元-关口-大邑断裂之间为前缘-褶皱冲断带,广元-关口-大邑断裂以东为前陆坳陷带,在构造变形特征上,各条断裂在演化上具有前展式特征,在松潘-甘孜构造带和韧性变形带构造变形强烈,形成推覆构造带等构造变形样式,在前缘-褶皱冲断带和前陆坳陷带,变形强度较弱,形成背冲断块或断层相关褶皱等构造,西北部区域的变形表现为塑性变形特征,向南东方向渐变为塑-脆性变形和脆性变形,在剖面上各条断裂所形成的深度向盆地方向逐渐递减。龙门山褶皱冲断带的分带性变形特征是由多种因素共同影响的结果,这些因素主要有板块构造背景的决定作用、多套滑脱层的控制作用和岩性因素的制约作用。
Based on the geological surveying and seismic data,we divided the Longmenshan fold and thrust zone into five tectonic belts,that is,the Songpan-Graze tectonic belt to the west of the Qingchuan-Maowen fault,the ductility deformation tectonic belt between Qingchuan-Maowen fault and Beichuan-Yingxiu fault,the basement involution fold and thrust belt between Beichuan-Yingxiu fault and Majiaoba-Tongjichang-Shuangshi fault,the front fold and thrust belt between Majiaoba-Tongjichang-Shuangshi fault and Guangyuan-Guankou-Dayi fault,and the foreland depression belt to the east of Guangyuan-Guankou-Dayi fault.Each fault is tectonically characterized with piggyback propagation,with intense tectonic deformation in the Songpan-Graze tectonic belt and the ductility deformation tectonic belt where nappe structure were well developed.The tectonic deformation was weak in the front fold and thrust belt and the foreland depression belt where pop-up,fault related fold and so on were developed widely.While the northwestern area displays the features of a ductile deformation and gradually changes to ductile-brittle deformation and brittle deformation to the southeast.The depth of each fault decreased toward the basin from the seismic section.Zonation of Longmenshan fold and thrust belt was affected by many factors,the main factors of which are the tectonic setting,multiple decollement layers and lithology.

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