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Isotope Dating of the Potash and Rock Salt Deposit at Bamnet Narong, NE-Thailand 被引量:8

Isotope Dating of the Potash and Rock Salt Deposit at Bamnet Narong, NE-Thailand
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摘要 Bamnet Narong is located in northeastern Thailand (Chaiyaphum Province). It is the largest salt mine in the country and has been mined for decades. The landscape in this part of Thailand is characterised by a low plateau, which is called the Khorat Plateau. The plateau is divided into two basins by the Phu Phan Range, the Sakhon Nakhon Basin in the north and the Khorat Basin in the south. The analysed potashes and rock salts are deposited in the Maha Sarakham Formation, which represents the salt-bearing strata of the Khorat Basin. The stratigraphic age of this deposit has been debated since the late 1960’s. The assigned ages range from Mid-Cretaceous to Late Cretaceous and up to the Eocene. In this study different isotopic dating systems (Rb-Sr, Sr-Sr, K-Ar and K-Ca) were applied. The stratigraphic age for the time of deposition was confirmed to be Mid Cretaceous (Cenomanian). Furthermore, the homogeneity of the carnallites was investigated in order to trace a possible redistribution of rubidium. Bamnet Narong is located in northeastern Thailand (Chaiyaphum Province). It is the largest salt mine in the country and has been mined for decades. The landscape in this part of Thailand is characterised by a low plateau, which is called the Khorat Plateau. The plateau is divided into two basins by the Phu Phan Range, the Sakhon Nakhon Basin in the north and the Khorat Basin in the south. The analysed potashes and rock salts are deposited in the Maha Sarakham Formation, which represents the salt-bearing strata of the Khorat Basin. The stratigraphic age of this deposit has been debated since the late 1960’s. The assigned ages range from Mid-Cretaceous to Late Cretaceous and up to the Eocene. In this study different isotopic dating systems (Rb-Sr, Sr-Sr, K-Ar and K-Ca) were applied. The stratigraphic age for the time of deposition was confirmed to be Mid Cretaceous (Cenomanian). Furthermore, the homogeneity of the carnallites was investigated in order to trace a possible redistribution of rubidium.
作者 Bent T. Hansen Klaus Wemmer Monique Eckhardt Prinya Putthapiban San Assavapatchara Bent T. Hansen;Klaus Wemmer;Monique Eckhardt;Prinya Putthapiban;San Assavapatchara(Geoscience Center Gottingen, University of Gottingen, Gottingen, Germany;Geoscience Programme, Kanchanaburi Campus, Mahidol University, Kanchanaburi, Thailand;Department of Mineral Resources, Bureau of Geological Survey, Bangkok, Thailand)
出处 《Open Journal of Geology》 2016年第8期875-894,共20页 地质学期刊(英文)
关键词 Isotope Dating Salt Deposits MID-CRETACEOUS Asian Potash Mine Thailand Isotope Dating Salt Deposits Mid-Cretaceous Asian Potash Mine Thailand
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