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三江中北段弧—盆格架与地质构造演化
引用本文:彭勇民,潘桂棠,罗建宁.三江中北段弧—盆格架与地质构造演化[J].四川地质学报,2000(3).
作者姓名:彭勇民  潘桂棠  罗建宁
作者单位:成都地质矿产研究所!四川成都610082
摘    要:弧—盆体系中岛弧与弧后盆地相间并存是一大特色。本文以昌都地区三叠纪弧—盆格局为例 ,阐明了岛弧、弧后盆地与夹于其间的微陆块等地质特征 ;划分出 2个构造演化阶段 ,一是早中三叠世江达—阿中岛弧与弧后盆地的发育 ,二是晚三叠世滞后型岛弧与生达残留弧后盆地的形成 ,并揭示了其演化的动力学。

关 键 词:弧—盆体系  构造演化  微陆块

ARC-BASIN FRAMEWORK AND GEOLOGIC-TECTONIC EVOLUTION IN MIDDLE-NORTHERN SECTOR OF THE JINSHA-NUJIANG-LANCANG RIVERS AREA
Peng,Yongmin,Pan,Guitang,Luo,Jianning.ARC-BASIN FRAMEWORK AND GEOLOGIC-TECTONIC EVOLUTION IN MIDDLE-NORTHERN SECTOR OF THE JINSHA-NUJIANG-LANCANG RIVERS AREA[J].Acta Geologica Sichuan,2000(3).
Authors:Peng  Yongmin  Pan  Guitang  Luo  Jianning
Abstract:Island arcs and basins coexist alternately This is characteristic of an arc basin system Exemplified by arc basin framework in Qamdo region,this paper expounds geological features of island arc,back arc basin and microcontinents between them and divides their tectonic evolution into 2 stages,i.e Early Middle Triassic Jamda Azhong island arc and back arc basin stage and Late Triassic Lagging island arc and Sinda relict back arc basin stage and reveals their evolutionary geodynamics
Keywords:arc  basin  system  tectonic  evolution  microcontinent
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