从多岛弧盆系构造看西特提斯造山系构造演化  

A brief review on the tectonic evolution of the west Tethysides

作　　者：袁四化 刘永江 常瑞虹 Franz Neubauer Johann Genser 关庆彬 黄倩雯 YUAN Sihua;LU Yongjiang;CHANG Ruihong;NEUBAUER Franz;GENSER Johann;GUAN Qingbing;HUANG Qianwen(College of Earth Sciences,Institute of Disaster Prevention,Sanhe 065201,Hebei,China;Frontiers Science Center for Deep Ocean Multispheres and Earth System,Key Lab of Submarine Geosciences and Prospecting Techniques,MOE,College of Marine Geosciences,Ocean University of China,Qingdao 266100,Shandong,China;Laboratory for Marine Mineral Resources,Qingdao National Laboratory for Marine Science and Technology,Qingdao 266237,Shandong,China;Paris-Lodron-University of Salzburg,Department of Geography and Geology,Geology Division,Hellbrunnerstrafie 34,5020 Salzburg,Austria;Hebei Key Laboratory of Earthquake Dynamics,Sanhe 065201,Hebei,China)

机构地区：[1]防灾科技学院地球科学学院,河北三河065201 [2]中国海洋大学深海圈层与地球系统前沿科学中心,海底科学与探测技术教育部重点实验室,海洋地球科学学院,山东青岛266100 [3]青岛海洋科学与技术国家实验室,海洋矿产资源评价与探测技术功能实验室,山东青岛266237 [4]萨尔茨堡大学地质与地理系,奥地利萨尔茨堡5020 [5]河北省地震动力学重点实验室,河北三河605201

出　　处：《沉积与特提斯地质》2021年第2期316-331,共16页Sedimentary Geology and Tethyan Geology

基　　金：国家自然科学基金项目(91755212;41772200);中央高校教师基金(ZY20110202);泰山学者(ts20190918);青岛市创新领军人才计划(19-3-2-19-zhc,41772200,91755212);防灾科技学院精品课程建设项目(Nos.JPJS2018001,JPJS2018005);国家重点研发计划项目(2016YFC0303902-04)。

摘　　要：本文通过综述近年西特提斯带主要缝合带的研究进展及所代表洋盆的发育特征,提出了古特提斯缝合带可能的位置和俯冲消亡方式。结合区域资料探讨了西特提斯带古生代末-中生代洋陆构造格局,认为东、西古特提斯洋完全可以类比,自晚古生代末西特提斯带主要受古特提斯大洋双向俯冲制约,在俯冲带后缘以二叠纪裂谷带为基础逐渐发展成中生代多岛弧盆系的新特提斯构造格局,西特提斯造山系主要表现为弧后洋盆消减造山作用。The research progress of the main suture zones in the west Tethysides and the development characteristics of the oceanic basin represented by them are reviewed.We propose the potential location of the Paleo-Tethys suture and summarize a brief evolution of the Paleo-Tethyan Ocean.Combining with regional geological data,this paper discusses the tectonic framework of the west Tethysides during the latest Paleozoic to the Mesozoic.The similar tectonic evolution is also found within the Paleo-Tethys which can be compared between the east and west parts.From the latest Paleozoic onward,the west Tethysides realm was mainly affected by doublesided subduction of the Paleo-Tethys.The Neo-Tethys was characterised by archipelagic arc-basin system during the Mesozoic,which succeed the Permian rifts in the aftermath of the Paleo-Tethys subduction.The west Tethysides was mainly manifested by the orogenesis of collaped back-arc basin.

关 键 词：多岛弧盆系 特提斯造山系 缝合带 洋板块地质 

分 类 号：P541[天文地球—构造地质学]