摘要
赣南上寒武统水石组风暴岩是在近年开展的鹅形圩幅１∶５万区调中首次发现的。文中对风暴岩沉积层序、剖面结构类型作了全面论述，并与理想风暴岩、浊积岩进行对比，初步探讨了风暴岩沉积模式，并指出了发现风暴岩的实际意义。
The storm rock in the Upper Cambrian Shuishi formation in SouthwestJiangxi was discovered for the first time in the regional geological surveyof“ Exing Wei”mapping( 1∶50,000) in the recent years. In this paper, theall-round describition has been made on the sedimentary sequence,thetypes of profile texture of the storm rock, and the comparison with theideal storm rock and turbidite has also been made. Meanwhile, the sedi- mentary model of the storm rock has been preliminarily discussed, andthe actual significance of the rock discovery has been pointed out.
出处
《江西地质》
1995年第1期21-27,共7页
Jiangxi Geology
