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香毛山一带下—中寒武统层序地层划分及盆地演化特征
引用本文:张彦杰,朱四宏,金霞,马惠萍.香毛山一带下—中寒武统层序地层划分及盆地演化特征[J].甘肃地质学报,2002,11(1):2-7.
作者姓名:张彦杰  朱四宏  金霞  马惠萍
作者单位:甘肃省地质调查院 甘肃兰州730000 (张彦杰),甘肃省地勘局第四勘查院 甘肃酒泉735000 (朱四宏,金霞),甘肃省地勘局第二勘查院 甘肃兰州730020(马惠萍)
基金项目:国土资源大调查项目“东湾、三道湾幅 1:5万区域地质调查”部分成果
摘    要:通过对香毛山一带早—中寒武世黑茨沟组岩石特征、沉积相和沉积构造环境等的调查研究 ,认为黑茨沟组沉积盆地属板内伸展机制下形成的裂谷微洋盆。根据相序变化特征、层序叠置形式、体系域组合特点及界面性质等将该套地层划分为 4个层序 ,并从盆地垂向沉积充填特征等方面探讨了盆地从形成—发展—成熟—萎缩闭合的演化过程。

关 键 词:香毛山一带  早—中寒武世黑茨沟组  层序地层  盆地演化

SEQUENCE STRATIGRAPHIC CLASSIFICATION AND BASIN EVOLUTION FEATURES OF LOWER-MIDDLE CAMBRIAN SERIES IN XIANGMAOSHAN DISTRICT
ZHANG Yan jie,ZHU Si hong,JIN Xia and MA Hui ping.SEQUENCE STRATIGRAPHIC CLASSIFICATION AND BASIN EVOLUTION FEATURES OF LOWER-MIDDLE CAMBRIAN SERIES IN XIANGMAOSHAN DISTRICT[J].Acta Geologica Gansu,2002,11(1):2-7.
Authors:ZHANG Yan jie  ZHU Si hong  JIN Xia and MA Hui ping
Institution:ZHANG Yan jie 1,ZHU Si hong 2,JIN Xia 2,MA Hui ping 3
Abstract:By studying on the rocks characteristices,sedimentary faces,sedimentary tectonic environment,ect, Heicigou Formation of early-middle Cambrian Epoch in the Xiangmaoshan district, we hold that sedimentary basin are belong to a rift valley micro-ocean basin, which formed during stretch mechanism of plate. According to the faces-change characteristices, the patent of sequence stratigraphic pile up, assemblage characteristices of system tract, boundary plane properties, ect, we have divided the series of stratigraphy into four sequences, while on the basis of sedimentary filled up basin features in the vertically,we have probed into the basin from sprout to development, mature, shrink close entirely process.
Keywords:In Xiangmaoshan district  Heicigou Formation of early  middle Cambrian Epoch  Sequence stratigraphic  Basin evolution features
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