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Geochemical simulation of the formation of brine and salt minerals based on Pitzer model in Caka Salt Lake 被引量:2
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作者 LIU Xingqi1, CAI Keqin2 & YU Shengsong3 1. Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China 2. China University of Geosciences, Beijing 100083, China 3. Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China 《Science China Earth Sciences》 SCIE EI CAS 2004年第8期720-726,共7页
The geochemical simulation of the formation of brine and salt minerals based on Pitzer model was made in Caka Salt Lake. The evolution of the mixed surface-water and the mineral sequences were calculated and compared ... The geochemical simulation of the formation of brine and salt minerals based on Pitzer model was made in Caka Salt Lake. The evolution of the mixed surface-water and the mineral sequences were calculated and compared with the hydrochemical compositions of the brine and the salt minerals of the deposit in Caka Salt Lake. The results show that the formation temperature of the lake is between 0°C and 5°C, which is well identical with other studies. The mixing of salt-karst water with the surface waters, neglected by the former researchers, is very important to the formation of the lake, indicating that the initial waters resulting in the formation of the lake are multi-source. It is the first time to use Pitzer model in China for making geochemical simulation of the formation and evolution of inland salt lake and satisfactory results have been achieved. 展开更多
关键词 Pitzer model Caka salt Lake geochemical simulation salt-karst water.
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青海省察尔汗盐湖盐溶研究 被引量:3
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作者 张兆广 李百贤 《盐湖研究》 CSCD 2008年第3期19-24,共6页
察尔汗盐湖是一个以卤水钾镁盐矿为主的大型的综合性盐类矿床,盐湖中有盐溶存在。主要从介绍水文地质背景开始来探讨盐溶的成因、分布规律、发展过程及对矿床的影响等问题。
关键词 盐溶 分布 形态 成因 发展 影响
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新疆库车西部古近系奥奇克盐底辟地质地貌特征及构造形成模式
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作者 杨梦莲 李江海 +2 位作者 王洪浩 陶崇智 章雨 《中国地质》 CAS CSCD 北大核心 2021年第1期129-138,共10页
库车前陆冲断带西部古近系奥奇克盐底辟是中国最典型的盐底辟构造,可作为盐构造研究的天然实验室。本文在前人研究的基础上,通过详细的野外填图,同时辅以遥感解译、地震解释和合成孔径雷达干涉测量(InSAR)技术,探讨了奥奇克盐底辟盐喀... 库车前陆冲断带西部古近系奥奇克盐底辟是中国最典型的盐底辟构造,可作为盐构造研究的天然实验室。本文在前人研究的基础上,通过详细的野外填图,同时辅以遥感解译、地震解释和合成孔径雷达干涉测量(InSAR)技术,探讨了奥奇克盐底辟盐喀斯特地貌特征,并分析了其形成机制及流变模式。奥奇克盐底辟表面盐喀斯特构造发育,在风化面上可见大量的溶洞、溶蚀冲沟构造,在新鲜面上可见梳状溶痕、微型峰丛等构造样式,此外,溶蚀坍塌等机械侵蚀构造也是本区常见的盐喀斯特构造类型。奥奇克盐底辟在形成过程中受逆冲断层、盐上地层的剥蚀作用、差异负载作用及盐岩自身的浮力作用的控制,共经历了逆冲盐底辟、侵蚀盐底辟、主动盐底辟和被动盐底辟4个主要阶段。盐岩喷出地表后,在重力作用下由核部向四周流动形成盐冰川,季节性河流的存在限制了盐底辟向东侧、东北侧及北侧传播,导致盐底辟呈现单侧增生的流变模式。 展开更多
关键词 库车前陆冲断带 奥奇克盐底辟 盐喀斯特 构造类型 地质调查工程 新疆
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