皖南浙西地区赫南特期沉积特征与沉积格局  

Sedimentary Characteristic and Framework of the Hirnatian Stage in the Southern Anhui and the Northern Zhejiang

作　　者：武国朋 校韩立[1] 

机构地区：[1]中国矿业大学(北京),北京100083

出　　处：《价值工程》2015年第7期310-311,共2页Value Engineering

基　　金：中国地质调查局项目;中国岩相古地理编图(编号:1212010916060)资助

摘　　要：由于潮坪相带只存在于扬子靠近华夏古陆的一侧,表明该时期华夏古陆已经推进到江绍断裂附近,而原江南古陆的位置附近存在盆地相的浊积岩,应为盆地环境,江南古陆在此时并未隆起。Because the tidal sedimentary depositional facies zone exists only in the one side of Yangtze near Cathaysia, the Cathaysia has advanced to near Jiangshao fracture, while the original location of the Jiangnan ancient land has the turbidite of the basin sedimentary facies which should be the basin environment, and the Jiangnan ancient land do not bulge at that time.

关 键 词：华夏古陆 江南古陆 赫南特期 扬子板块 

分 类 号：P512.2[天文地球—地质学]