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Organic Facies Characteristics of the Triassic Ispartacay Formation, Antalya Nappes, Western Taurus, Turkey

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dc.creator Kuscu, Mustafa
dc.creator Unal, Neslihan
dc.creator Hokerek, Selin
dc.creator ÖZÇELİK, ORHAN
dc.creator ALTUNSOY, MEHMET
dc.date 2014-12-31T22:00:00Z
dc.date.accessioned 2020-10-06T09:15:54Z
dc.date.available 2020-10-06T09:15:54Z
dc.identifier 01597118-a165-4956-99e5-98d7b6ece677
dc.identifier 10.1016/j.proeps.2015.08.055
dc.identifier https://avesis.sdu.edu.tr/publication/details/01597118-a165-4956-99e5-98d7b6ece677/oai
dc.identifier.uri http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/51980
dc.description In the Antalya Nappes (SW Turkey), the Triassic Ispartacay Formation consists of radioaria, chert, turbiditic limestone and sandstone. Detailed data from thick Triassic sediments (Ispartacay Formation) made it possible to construct an organic facies framework using different zonation. Organic matter is composed predominantly of woody material, with a minor contribution of planty and woody material. Kerogen in the deposits is type III, as indicated by organic petrographic observations and Rock-Eval data. Total organic carbon (TOC) values are generally between 0.16 and 1.36 %, but reach 5.24 % in the formation. Tmax values vary between 331 and 602 degrees C, confirming the increase in maturation trends indicated by vitrinite reflectance data. Organic facies type D was identified in the investigated units. Organic facies D is related to sandstone and limestone litofacies. This facies is characterized by average values of HI around 18 (equivalent to type III kerogen), TOC around 0.85 %, and an average of S2 of 0.19 mg HC/g of rock. The organic matter is highly oxidized, decomposed and reworked. Organic facies D is no generative. (C) 2015 Published by Elsevier RV.
dc.language eng
dc.rights info:eu-repo/semantics/closedAccess
dc.title Organic Facies Characteristics of the Triassic Ispartacay Formation, Antalya Nappes, Western Taurus, Turkey
dc.type info:eu-repo/semantics/conferenceObject


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