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甘肃昌马地区寒武纪构造演化探讨
引用本文:黄增保, 金霞. 甘肃昌马地区寒武纪构造演化探讨[J]. 西北地质, 2004, 37(1): 51-57.
作者姓名:黄增保  金霞
作者单位:甘肃省地勘局第四地勘院, 甘肃 酒泉 735000
基金项目:中国地质调查局区域地质调查项目(200213000020)《1∶25万红宝石幅》区调成果
摘    要:位于北祁连山造山带西段的昌马地区,1:5万东湾、三道湾幅区调在中寒武世地层中发现Leiosphaeridia,Lophosphaeridium,Cymatiosphaera,Retisphaeridium,Synsphaeridium,Multiplicis-phaeridium,Retinarites等晚震旦世的藻类化石。据此,笔者将本区中寒武世地层解体为3部分:晚震旦世地层、早寒武世地层和中寒武世黑茨沟组。并对锅底坑蛇绿混杂岩带进行了确认,在此基础上对本区寒武纪构造演化模式作以探讨。

关 键 词:构造演化   蛇绿混杂岩   昌马地区   地层划分
文章编号:1009-6248(2004)01-0051-07
收稿时间:2003-05-23
修稿时间:2003-05-23

Structural evolution of Cambrian tectonic belt in Changma area,Gansu
HUANG Zen-bao, JIN Xia. Structural evolution of Cambrian tectonic belt in Changma area, Gansu[J]. Northwestern Geology, 2004, 37(1): 51-57.
Authors:HUANG Zen-bao  JIN Xia
Affiliation:Fourth of Gansu Institute of Geology and Mineral Exploration, Jiuquan 735000, China
Abstract:In the west Qilian orogenic belt of Changma, Gansu,Late Sinian fossils,e.g: Leiosphaeridia,Lophosphaeridium,Cymatiosphaera,Retisphaeridium,Synsphaeridium,Multiplicisphaeridium,Retinarites et al. were discovered in Heicigou Formation of the Middle Cambrian through 1:50 000 geological mapping.Based on this reseach,the Middle Cambriam strata was divided three parts:Late Sinian strata,Early Cambriam strata,and Heicigou Formation of the Middle Cambriam and structural evolution model from the Late Sinian to the end of the Middle Cambrian was put forward.
Keywords:stractural evolution  ophiolitic melange  Changma area  stratigraphic division
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