首页> 外文期刊>Open Journal of Geology >Lithostratigraphy of the Late Cretaceous Khao Ya Puk Formation in Nakhon Thai Region, Thailand: Implication for Depositional Environment
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Lithostratigraphy of the Late Cretaceous Khao Ya Puk Formation in Nakhon Thai Region, Thailand: Implication for Depositional Environment

机译:泰国那空府地区晚白垩世Khao Ya Puk组岩性地层学:对沉积环境的影响

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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.
机译:Khao Ya Puk组(> 400 m厚)在泰国那空地区暴露良好,分为三个部分。考亚普克组一致地覆盖在上岩盐玛哈沙拉堪组的硬石膏层顶部。反过来,它被普卡特组覆盖不整合。考亚普克组被认为是白垩纪晚期干旱气候内陆地下的淡水湖区沉积。从岩石地貌上看,考亚普克组可以与沉积在霍拉特高原的霍拉特-乌汶盆地和乌冬-萨空盆地的富托克组相关。

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