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Facies analysis and dynamic depositional modelling of the upper permian chhidru formation,salt range,upper indus basin,Pakistan
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نویسنده
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ahmad s. ,waqas m. ,khan s.s. ,farooq swati m.a. ,jan i.u. ,ali f. ,yaqoob m. ,sadiq a. ,khan s. ,ibad-ur-rehman department of geology
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منبع
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journal of himalayan earth sciences - 2015 - دوره : 48 - شماره : 1 - صفحه:64 -80
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چکیده
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In this paper we have used the outcrop data and utilized facies analysis techniques for the dynamic depositional modeling of chhidru formation,exposed in the nammal gorge and the chhidru nala sections in the salt range,upper indus basin of pakistan. based on the integrated eld and petrographic criteria,ve different facies types i.e.,chf-1-chf-5 are recognized. the chf-1 corresponds to the sandy limestone interbedded with clays facies while chf-2 is a medium bedded sandy limestone facies. the chf-3 is represented by the massive sandy limestone facies. the chf-4 (calcareous sandstone facies) and chf-5 (thick bedded to massive white sandstone facies) have been identied in the upper part of the two stratigraphic sections. the depositional characteristics of these facies are consistent with the proximal inner shelf to distal middle shelf settings of a siliciclastic-carbonate mixed platform. based on the integration of the outcrop data,facies information and fusulinid biostratigraphy the dynamic depositional model of the chhidru formation is presented. the new data enabled identication of two (02) 3rd order transgressive-regressive depositional sequences. the rst transgressive sequence consists of the transgressive systems tract (tst 1) that further constitutes six parasequences. the second transgressive depositional sequence constitutes the second transgressive systems tract (tst 2) with no signicant parasequence. the chronologic calibration fusulnid biostratigraphic age of the chidru formation suggest that deposition of the at the base tst 1 started at 252.5 ma and the topmost beds of tst 2 corresponds to 253.8 ma,respectively. the global comparison of the relative sea level during 252.5-253.8 ma shows prominent eustatic signatures,however the ooding surfaces bounding the parasequences are ascribed to the local tectonics. © 2015 national centre of excellence in geology. all rights reserved.
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کلیدواژه
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Pakistan; Sequence stratigraphy; Shelf; Upper permian
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آدرس
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department of geology, Pakistan, department of geology, Pakistan, department of geology, Pakistan, department of geology, Pakistan, national centre of excellence in geology, Pakistan, department of geology, Pakistan, department of geology, Pakistan, department of geology, Pakistan, department of geology, Pakistan
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Authors
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