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Lithostratigraphy of the Late Cretaceous Khao Ya Puk Formation in Nakhon Thai Region, Thailand: Implication for Depositional Environment
Office of Mineral Resources Region 2, Department of Mineral Resources, Ministry of Natural Resources and Environment, Khon Kaen, Thailand
Department of Geotechnology, Faculty of Technology, Khon Kaen University, Khon Kaen, Thailand
- 1 Office of Mineral Resources Region 2, Department of Mineral Resources, Ministry of Natural Resources and Environment, Khon Kaen, Thailand
- 2 Department of Geotechnology, Faculty of Technology, Khon Kaen University, Khon Kaen, Thailand
Open Journal of Geology·Volume 09 (2019)·Pages 711–713·Published 20 September 2019·DOI10.4236/ojg.2019.910082
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Abstract
The Khao Ya Puk Formation (>400 m thick) is well exposed in the Nakhon Thai Region, and is subdivided into three members. The Khao Ya Puk Formation overlies conformably on top of the anhydrite layer of the upper rock salt Maha Sarakham Formation. In turn, it is overlain unconformably by the Phu Khat Formation. The Khao Ya Puk Formation is interpreted to have been deposited by freshwater lake area in arid climate inland subkha in the Late Cretaceous. Lithostatigraphically, Khao Ya Puk Formation can be correlated with the Phu Tok Formation that has been deposited in the Khorat-Ubon basin and Udon-Sakon basin of the Khorat Plateau.
KeywordsKhao Ya Puk FormationNakhon Thai RegionLithostratigraphy
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