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甘肃敦煌-北山早前寒武纪岩石组合-构造初步框架
引用本文:梅华林,于海峰,李铨,左国朝.甘肃敦煌-北山早前寒武纪岩石组合-构造初步框架[J].地质调查与研究,1997(4).
作者姓名:梅华林  于海峰  李铨  左国朝
作者单位:地矿部天津地质矿产研究所!天津300170(梅华林,于海峰,李铨),甘肃地质矿产局!兰州730000(左国朝)
基金项目:“九五”地矿部资源与环境科技攻关课题!95—02—011—02
摘    要:甘肃敦煌-北山地区广泛出露早前寒武纪岩石。这些岩石在早期的《甘肃省区域地质志》中被确定为前长城系、长城系、奥陶-志留系及部分石炭系。本文认为这些岩石应属太古宙和古元古代。据此,重新厘定了该区早前寒式纪岩石-构造框架。自南向北划分为敦煌太古宙杂岩区、北山南带古元古代剪切构造区和北山北带古元古代-太古宙杂岩区,并根据变形特点和岩石组合,进一步划分出次级带。

关 键 词:岩石-构造分区  早前寒武纪  敦煌-北山地区

PRELIMINARY LTTHO-TECTONIC FRAMEWORK OF EARLY PRECAMBRIAN ROCKS IN DUNHUANG-BEISHAN AREA,GANSU, WEST CHINA
Met Hualin, Yu Haifeng ,and Liquan.PRELIMINARY LTTHO-TECTONIC FRAMEWORK OF EARLY PRECAMBRIAN ROCKS IN DUNHUANG-BEISHAN AREA,GANSU, WEST CHINA[J].Geological Survey and Research,1997(4).
Authors:Met Hualin  Yu Haifeng  and Liquan
Abstract:Early - Precambrian rocks are widely exposed in Dunhuang-Beishan area, GansuProvince. The Precambrian rocks are traditionally defined as strata of Pre-Changchengian,Ordovician-Silurian, Carboniferous and Baihu Group. According to field investigation, the rocksare reinterpreted as Aichaean and Palaeoproterosoic ages. They can be divided into three terrainsfrom south to north: Dunhuang mctamorphic terrain, south Beishan palaeoproterozoic tectonicterrain and north Beishan Archaean-Palaeoproterozoic terrain. These terrains can be furtherdivided into litho-structural zones(belts) according to deformation ard metamorphism, that is:Hongliuxia-Dunhuang Metasedimentary Belt, Anxi-Cijin TTG Belt, Baidunzi-Qiaowan Shearsone within the Dunhuang terrain; Xiaoxigong-Sishilijing Palaeoproterozoic shear zone andYamajie-Mazongshan Palaooproterozoic Shear zone within the south Beishan.
Keywords:Litho-tectonic Framework  Precambrian  Dunhuang-Beishan area  
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