ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
成盐理论引领我国找钾取得重要进展
  
关键词:salt formation theory  potash deposit prospecting  gravel brine in Qaidam basin  Kuqa depression of Tarim  Paleogene potash-bearing ore beds  Triassic polyhalite  “two-storey” potash-forming model  Ordovician salt basin
基金项目:中国地质调查局地质大调查项目“油钾兼探实施方案和调查评价部署”(编号: 1212011085524);NSFC-云南联合重点基金项目(编号: U0833601)
作者单位E-mail
郑绵平 中国地质科学院矿产资源研究所, 国土资源部盐湖资源与环境重点实验室 zhengmp2010@126.com 
侯献华 中国地质科学院矿产资源研究所, 国土资源部盐湖资源与环境重点实验室  
于常青 中国地质科学院地质研究所  
李洪普 青海省柴达木综合地质矿产勘查院  
尹宏伟 南京大学地球科学与工程学院  
张震 中国地质科学院矿产资源研究所, 国土资源部盐湖资源与环境重点实验室  
邓小林 中化地质矿山总局地质研究院  
张永生 中国地质科学院矿产资源研究所, 国土资源部盐湖资源与环境重点实验室  
郭廷峰 青海省柴达木综合地质矿产勘查院  
韦钊 中化地质矿山总局地质研究院  
王绪本 成都理工大学  
安莲英 成都理工大学  
乜贞 中国地质科学院矿产资源研究所, 国土资源部盐湖资源与环境重点实验室  
谭筱虹 云南省地质调查院  
张雪飞 中国地质科学院矿产资源研究所, 国土资源部盐湖资源与环境重点实验室  
牛新生 中国地质科学院矿产资源研究所, 国土资源部盐湖资源与环境重点实验室  
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摘要:
The Leading Role of Salt Formation Theory in the Breakthrough and Important Progress in Potash Deposit Prospecting
      The salt formation theory has led to the breakthrough and important progress in potash deposit prospecting: a new type gravel brine layer rich in potassium was discovered in the early pre-Quaternary strata in Altun Mountains in the west of Qaidam Basin. This progress was made by the Salt Party of the Institute of Mineral Resources, Chinese Academy of Geological Sciences, headed by Professor ZhengMianping, academician of the Chinese Academy of Engineering, with such institutions as the Qaidam Comprehensive Exploration Institute of Geology and Mineral Resources as the co-researchers and under the joint support of geological survey projects and key projects of the National Natural Science Foundation of China. Drilling shows that it possesses the estimated resource quantity of 350 million tons and hence is likely to be the reserve base of potash salt in Qaidam Basin. Additionally, Paleogene potash-bearing ore beds with the thickness of 100 meters were found in Kuqa depression, Tarim, where there is a 41 meter-thick salt bed of potassium chloride that reaches industrial grade. Furthermore, Triassic polyhalite was found in Sichuan Basin, which is not only an important potassium source in deep brine rich in potash but also a precious slow-release potassium fertilizer. Besides, in Upper Yangtze River Basin, 13 potassium-rich brine deposits of brine-bearing structure were evaluated, and the potassium chloride resource is estimated to be 49.17 million tons. What is more, in Mengyejing of southwestern Yunnan Province, a “two-storey” potash-forming model was set up, and, in Ordovician salt basin of northern Shaanxi Province, the area of potash prospecting target area has been largely reduced, which shows the dawn of the breakthrough in marine potash prospecting.
ZHENG Mian-ping,HOU Xian-hua,YU Chang-qing,LI Hong-pu,YIN Hong-wei,ZHANG Zhen,DENG Xiao-lin,ZHANG Yong-sheng,GUO Ting-feng,WEI Zhao,WANG Xu-ben,AN Lian-ying,NIE Zhen,TAN Xiao-hong,ZHANG Xue-fei,NIU Xin-sheng.2015.The Leading Role of Salt Formation Theory in the Breakthrough and Important Progress in Potash Deposit Prospecting[J].Acta Geoscientica Sinica,36(2):129-139.
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