{ "labelLang" : "hun", "responseDate" : "2024-03-28 21:24", "content" : { "otype" : "JournalArticle", "mtid" : 31095537, "status" : "VALIDATED", "published" : true, "comment" : "Funding Agency and Grant Number: Scientific and Technological Research Council of Turkey (TUBITAK) [YDABCAG-16Y383]\n Funding text: A part of this study was supported by the Scientific and Technological Research Council of Turkey (TUBITAK) under a project (YDABCAG-16Y383) entitled with \"Mineralogical and petrographical composition of the different lithotypes in the Kinik coals and the determination of their porosity character using X-ray micro-CT, Soma Basin (Turkey)\". A. Karayigit and R.G. Oskay collected coal samples from Kink coalfield and performed the petrographical, SEM and mineralogical examinations. A. Bechtel conducted Rock-Eval pyrolysis and biomarker analyses. R.G. Oskay, A. Karayigit and A. Bechtel interpreted the data and prepared the paper. The authors would like to thank Muzaffer Polat, and Polyak Eynez Corp. for the permission of sampling and Feridun Emre Yagimh and Ali Tiirkoglu (Polyak Eynez Corp.) for their support during field study, and to Dr. Carley Johnson for her assistance during manuscript preparation. 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This study presents the coal-petrographical, mineralogical and organic geochemical features of samples collected from two deep cores. Samples from seam kM2 generally display low ash yields and high TOC content, whereas the kM3 and kP1 seams are characterized by relatively high ash yields and low TOC values. Furthermore, total S content of the kP1 is very high (up to 7.0%, on dry basis). The maceral composition, the coal facies diagrams, and the distributions of n-alkanes and diterpenoids indicate changes of depositional conditions and vegetation in the palaeomires of the kM2 seam during Early Miocene. The precursor peat of kM2 seam started accumulating under limnotelmatic conditions followed by pure telmatic ones. 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