| 白强.泰国呵叻盆地沉积演化特征及钾镁盐矿成因[J].矿产勘查,2020,11(2):365-368 |
| 泰国呵叻盆地沉积演化特征及钾镁盐矿成因 |
| Characteristics of sedimentary evolution and origin of K-Mg salt in Khorat Basin, Thailand |
| 投稿时间：2020-01-21 |
| DOI： |
| 中文关键词: 钾镁盐矿 沉积特征 成因 呵叻盆地 泰国 |
| 英文关键词: potassium salt,sedimentary characteristics,origin,Khorat Basin,Thailand |
| 基金项目: |
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| 中文摘要: |
| 泰国呵叻盆地KCL远景储量高达430亿t。 本文分析了呵叻盆地已有地质资料及近年来钾镁盐矿勘查成果,剖析了呵叻盆地的沉积演化特征,并对区内钾镁盐矿成因进行了分析。认为呵叻盆地经历了3个阶段的沉积,区内马哈沙拉堪组为主要含盐岩系,钾镁盐矿属“海源陆相”成因。 |
| 英文摘要: |
| Analytic studied on geological information and the results of K-Mg potassium prospection in recent years,Analyzed Characteristics of sedimentary evolution in Khorat basin,And analyzed the causes of the potassium and magnesium salt deposits in the region. Believed that Khorat basin has undergone threes stages of deposition,The Mahasalakan Formation is the main salt forming rock,And the causes of potassium magnesium deposit is“Sea source continental facies”. |
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