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班公湖-怒江结合带西段中特提斯多岛弧构造演化
引用本文:曹圣华,邓世权,肖志坚,廖六根.班公湖-怒江结合带西段中特提斯多岛弧构造演化[J].沉积与特提斯地质,2006,26(4):25-32.
作者姓名:曹圣华  邓世权  肖志坚  廖六根
作者单位:1. 中国地质大学,地球科学学院,湖北,武汉,430074;江西省地质调查研究院,江西,南昌,330030
2. 江西省地质调查研究院,江西,南昌,330030
基金项目:中国地质调查局“1∶25万邦多区幅、措麦区幅、羌多幅、日土县幅、喀纳幅(国内部分)区域地质调查”
摘    要:本文根据1∶25万地质填图成果,将班公湖-怒江结合带西段弧-盆系时空结构自北向南划分为五峰尖-拉热拉新晚侏罗世—早白垩世陆缘火山-岩浆弧带、班公湖蛇绿混杂岩北、南亚带和昂龙岗日-班戈白垩纪—始新世岩浆弧带等,初步认为中特提斯洋经历了三叠纪—早侏罗世扩张,中—晚侏罗世往北、南双向俯冲,晚三叠世—早白垩世残余洋(海)盆和早—晚白垩世陆-弧(陆)碰撞等演化阶段。

关 键 词:班公湖-怒江结合带  中特提斯  多岛弧-盆系  构造演化  西藏
文章编号:1009-3850(2006)04-0025-08
收稿时间:2006-08-21
修稿时间:2006-08-21

The archipelagic arc tectonic evolution of the Meso-Tethys in the western part of the Bangong Lake-Nujiang suture zone
CAO Sheng-hu,DENG Shi-quan,XIAO Zhi-jian,LIAO Liu-gen.The archipelagic arc tectonic evolution of the Meso-Tethys in the western part of the Bangong Lake-Nujiang suture zone[J].Sedimentary Geology and Tethyan Geology,2006,26(4):25-32.
Authors:CAO Sheng-hu  DENG Shi-quan  XIAO Zhi-jian  LIAO Liu-gen
Institution:1. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China ; 2. Jiangxi Institute of Geological Survey, Nanchang 330030, Jiangxi, China
Abstract:The spatial-temporal framework of the arc-basin systems in the western part of the Bangong Lake-Nujiang suture zone may be divided, from north to south on the basis of the results of the 1:250 000 geological mapping, into the Wufengjian-Larelaxin Late Jurassic-Early Cretaceous epicontinental volcanic-magmatic arc zone, northern and southern subzones of the Bangong Lake ophiolitic mélange zone, and Nganglong Kangri-Baingoin Cretaceous-Eocene magmatic arc zone. The Meso-Tethyan Ocean once went through the Triassic-Early Jurassic spreading, Middle-Late Jurassic northward and southward bidirectional subduction, Late Triassic-Early Cretaceous residual ocean (sea)basin and Early-Late Cretaceous continent-arc (continent)collision.
Keywords:Bangong Lake-Nujiang suture zone  Meso-Tethys  archipelagic arc-basin system  tectonic evolution  Xizang
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