摘要
石盐矿床在蒸发沉积过程中经受环境变化而被改造 ,兰坪 -思茅盆地石盐矿床石盐矿物流体包裹体特征及测温数据证明 ,该区地壳在喜山期一直处于活动状态 ,在石盐的成矿、成矿期后都迭加了火山以及构造
Salt evaporate deposits usually were alterred by environment change in salt lake evaporate depositing. During the salt deposit forming, Lanpin simao basin salt evaporate deposits were borne volcanic action. Tectonism hotspot action becauce the area still crust movement in Cenozoic Era.Those salt formation are discussed by studied salt mineral flnid inclusion at this paper.
出处
《矿产与地质》
2001年第2期113-115,共3页
Mineral Resources and Geology
基金
广西青年科学基金资助项目
