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CHEMICAL COMPOSITION OF THE ANCIENT LAKE AT JINTAN SALT MINE:EVIDENCE FROM FLUID INCLUSIONS IN HALITE
Author(s): MENG Fanwei1, 2), NI Pei 2), YAN Xianqin3), WANG Tiangang2), YAN Kui1), WANG Guoguang2), ZHAO Chao2) and SONG Weimin 4)1) State Key Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology andPalaeontology Chinese Academy of Sciences, Nanjing 2100832) State Key Laboratory for Mineral Deposit Research, Institute of Geo-Fluids, School of Earth Sciences and Engineering, Nanjing University, Nanjing 2100933) Jiangsu Institute of Geology and Mineral Resources, Nanjing 2100184) East China Mineral Exploration &Development Bureau, Nanjing 210007
Pages: 75-
79
Year: 2011
Issue:
3
Journal: Acta Micropalaeontologica Sinica
Keyword: 包裹体; 低温冷冻扫描电镜-能谱法; Mg/Ca; 金坛盐矿; 江苏;
Abstract: 我国白垩纪晚期—古近纪由于燕山运动和喜马拉雅运动,形成了一系列的断陷盆地,金坛盐矿就是该时期始新世中晚期的盐湖沉积。本次研究首次在国内半定量的进行了石盐原生包裹体的分析,发现其中Ca2+缺失而富含SO42-,原始卤水成分为Na-Mg-K-Ca-Cl-SO4体系。
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