摘要
通过野外剖面实测和镜下薄片鉴定分析,对库鲁克塔格地区寒武系莫合尔山组发育的风暴沉积物进行了研究。根据风暴沉积物结构、粒屑的形状及颜色的差别将本地区的风暴沉积物划分为四种类型的风暴岩,分别是原地风暴粗粒灰岩、异地型风暴粗颗粒灰岩、丘状交错层理灰岩和风暴浊积灰岩。这四种类型的风暴岩由陆向海发育于台地前斜坡到浅海陆棚的广阔的浅海环境中。
The paper made research on developed storm sediment of Cambrian Moheershan formation in Kuruktag areathrough field profile actual measurement and microscopical thin section analysis,According to the structure,grain dust shape and color difference of storm sediment ,storm rock of the study are has been grouped as four types,which are situ storm coarse-grained rock,remote-type storm coarse par-ticle rock,hummocky cross rock and storm turbidity rock. These four types of storm rocks developed in the plateau land from the sea-front slope to the shallow shelf of a vast shal-low sea environment.
出处
《石油地质与工程》
CAS
2010年第1期23-26,共4页
Petroleum Geology and Engineering
基金
中国石化西部勘探开发项目(项目编号XBKT2003KY10003)
