《Table 1 Summary of the characteristic features of the lithofacies types in the Dasht Murgha Group,

《Table 1 Summary of the characteristic features of the lithofacies types in the Dasht Murgha Group,   提示：宽带有限、当前游客访问压缩模式
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《"A Paleogeographic and Depositional Model for the Neogene Fluvial Succession, Pishin Belt, Northwest Pakistan: Effect of Post Collisional Tectonics on Sedimentation in a Peripheral Foreland Setting"》


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Ten stratigraphic sections at outcrop were studied and logged in detail across the Pishin Belt.Twelve distinct lithofacies were identified and grouped into four facies associations（Table 1）.The descriptive terminology and facies codes of Miall（1978，1996）and Arenas and Pardo（1999）have been used.However，facies and facies associations were defined，classified and interpreted using the classification schemes of Ashley（1990），Bridge（1993），Miall（1978，1985，1992，1996）and Hjellbakk（1997）（Table 2） .Bed thickness has been categorized according to the classification scheme of Ingram（1954），and grain size according to the classification scheme of Wentworth（1922）.

图表编号XD0017169900    严禁用于非法目的
绘制时间2018.04.01
作者Aimal K.KASI、Akhtar M.KASSI、Muhammad UMAR、Henrik FRIIS、Mohibullah MOHIBULLAH、Razzaq A.MANAN
绘制单位Centre of Excellence in Mineralogy, University of Balochistan、Department of Geology, University of Balochistan、Department of Geology, University of Balochistan、Department of Earth Sciences, COMSATS Institute of Technology、Department of Geoscience, Aarhus
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