论浊流、风暴流、等深流沉积特征  

On the Sedimentary Characteristics of Turbidity Current,Storm Current and Isobath Current

作　　者：马丽 周仕林 王钦 MA Li;ZHOU Shilin;WANG Qin(College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China)

机构地区：[1]成都理工大学地球科学学院,四川成都610059

出　　处：《四川有色金属》2021年第2期3-7,共5页Sichuan Nonferrous Metals

摘　　要：浊流是密度流的一种,由沉积物与水混杂形成。风暴流是风暴在滨岸和海底引起的一种特殊流动状态,风暴的退潮流可以产生向海流动的密度流,并形成粒序层沉积。等深流是因为地球自转的结果而构成的温盐水循环底流。Turbidity current is a density current of sediment mixed with water.The storm current is a special flow state caused by the storm on the shore and the sea bottom.The storm ebbing current can produce the density current flowing to the sea and form the grain sequence deposition.The isobath flow is the result of the circulation of hot brine by the Earth’srotation.

关 键 词：浊积岩 沉积特征 风暴岩 重力流 

分 类 号：P618[天文地球—矿床学]