泰国暖颂钾盐矿床粗粒岩盐沉积特征及其成因研究  

Characteristics and Origin of Coarse Halite in the First Sedimentary Cycle of the Potash Deposit,Non Sung District,Nakhon Ratchasima Province,Thailand

作　　者：方龙 秦占杰[1,2] 石国成 李庆宽 朱登贤 李强 都永生 袁秦[1,2] 张西营 山发寿[1,2] FANG Long;QIN Zhanjie;SHI Guocheng;LI Qingkuan;ZHU Dengxian;LI Qiang;DU Yongsheng;YUAN Qin;ZHANG Xiying;SHAN Fashou(CAS Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources,Qinghai Institute of Salt Lakes,Chinese Academy of Sciences,Xining,810008,China;Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes,Xining,810008,China;University of Chinese Academy of Sciences,Beijing,100049,China;Laos Qinghai Engineering Technology Co.,Ltd,Vientiane,01000,Laos;International Petroleum Group Co.,Ltd,Bangkok,10320,Thailand;Qinghai Salt Lake Industry Corporation Resources Branch,Golmud,816000,China)

机构地区：[1]中国科学院青海盐湖研究所,中国科学院盐湖资源综合高效利用重点实验室,青海西宁810008 [2]青海省盐湖地质与环境重点实验室,青海西宁810008 [3]中国科学院大学,北京100049 [4]老挝青海工程技术有限公司,老挝万象01000 [5]泰国国际石油集团有限公司,泰国曼谷10320 [6]青海盐湖工业股份公司资源分公司,青海格尔木816000

出　　处：《盐湖研究》2024年第1期107-119,共13页Journal of Salt Lake Research

基　　金：国家自然科学基金项目(42072097)、中国科学院青年创新促进会人才项目(2021431)、中国科学院国际合作局“一带一路”专项项目(122363KYSB20190033)、青海省“昆仑英才·高端创新创业人才”计划团队项目、青海省地质矿产勘查开发局地勘项目“钾盐探测方法技术及成矿机理研究”。

摘　　要：老挝-泰国呵叻高原钾盐矿床储量大、品位高、易开发,粗粒岩盐在该钾盐矿床中普遍发育,其对水成盐转化、水体掺杂过程、钾盐富集演化等沉积环境具有重要的指示作用,然而,关于其成因至今仍未有详细报道。利用岩石学、显微岩相学和沉积学方法对呵叻高原西南部暖颂县钾盐矿床钻孔岩芯第一沉积旋回粗粒岩盐的成因进行了研究,得到如下结论:(1)粗粒岩盐主要有3种成因,浅水环境中蒸发浓缩阶段原生生长,浅水环境中干盐湖阶段胶结生长,埋藏环境中孔隙卤水重结晶生长;(2)根据粗粒岩盐的成因、沉积规律和钻孔岩性特征可将马哈萨拉堪组下盐层沉积演化划为5个沉积阶段:岩盐沉积稳定阶段、岩盐沉积过渡阶段、光卤石沉积初期阶段、光卤石沉积稳定阶段和次生岩盐沉积阶段;(3)研究区钾盐矿床整体的沉积环境为浅水。粗粒岩盐在矿层中的赋存特征、成因以及与其它岩相的组合特征共同表明了钾盐在沉积过程受到了不同程度的淡水稀释和埋藏后的改造作用。Potash deposit in Laos-Thailand Khorat Plateau is characterized by large reserves,high grade,and easy to exploitation.Coarse halite crystalsare widely distributed in this potash deposit,which plays an important role in revealing the sedimentary environment such as water-salt transformation,paleo-hydrodynamic conditions,potash sedimentation,etc.In this paper,the origin and geological significance of coarse halite crystals in the first sedimentary cycle of the potash deposit in Non Sung district,southwest of Khorat Plateau were discussed.The following understandings were obtained:(1)Coarse halite crystals mainly have three origins,including primary growth in the concentration stage in shallow water environment,cemented growth in desiccation stage in shallow water environment,and recrystallized growth of pore brine in burial environment;(2)the sedimentary evolution of the first sedimentary cycle in the Mahasarakham Formation in the study area can be divided into five depositional stages from bottom up:stage of halite stable deposition,stage of halite-transit-to-carnallite,early stage of carnallite deposition,stage of carnallite stable deposition,and stage of secondary halitedeposition;(3)The sedimentary environment of the potash deposit in the study area is shallow water.The occurrence characteristics,and lithofacies of coarse halite crytals in the potash layer indicate that the potash deposit has been diluted by relatively fresh water during the deposition process and experienced diagenetic process.

关 键 词：粗粒岩盐 岩相学 钾盐 暖颂 呵叻高原 

分 类 号：P619.211[天文地球—矿床学]