中国东南地区中新生代岩盐矿床的沉积成盐特征  

Sedimentary and Salt Forming Characteristics of Meso-Cenozoic Halite Deposits in Southeast China

作　　者：杨吉根[1] 

机构地区：[1]华东地质学院,抚州市344000

出　　处：《盐湖研究》1993年第4期1-8,共8页Journal of Salt Lake Research

摘　　要：本文简介了中国东南地区新生代岩盐矿床的一般概况,着重从七个方面阐述了岩盐矿床形成过程中的沉积成盐特征,对这些沉积成盐特征的了解有助于该地区岩盐矿床的研究。In addition to a brief introduction to the jeneral characteristics of Meso-Cenezoic halite deposits in Southeast China, the paper, in seven sections, emphasizes the expounding sedimentary and salt-forming characteristics during the formation of these deposits, and also points out that this type of work is favorable to the investigation of halite deposits in the region.

关 键 词：岩盐矿床 成盐特征 岩盐 沉积成盐 

分 类 号：P619.211[天文地球—矿床学]