THE SECOND PALEOZOIC COAL OF TURKEY, DIYARBAKIR-HAZRO COALS AND THEIR PROPERTIES

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dc.contributor.authorKavak, Orhan
dc.contributor.authorToprak, Selami
dc.date.accessioned2024-04-24T17:47:42Z
dc.date.available2024-04-24T17:47:42Z
dc.date.issued2012
dc.departmentDicle Üniversitesien_US
dc.description12h International Multidisciplinary Scientific Geoconference (SGEM) -- JUN 17-23, 2012 -- Albena, BULGARIAen_US
dc.description.abstractThis study was carried out in Hazro-Diyarbakir region (SW of Turkey), which owns a very unique coal formation. Aside from Zonguldak region (NW of Turkey), Paleozoic coal formations are very rare in Turkey. Hazro region comprises the oldest units of the region which was outcropped due to a considerably spectacular form of an anticline. Diyarbakir-Hazro occurrences are outcropped within the Hazro anticline. The anticline was emerged through a vast Tertiary Basin in the area. Gomaniibrik Formation, of Upper Permian age, is the main formation of the region. The formation which contains of shale, sandstone succession and is of lacustrine type formation comprises of two important coal levels. Chemical and petrographic analyses of the coals were taken into consideration. Coal quality investigation along with proximate (moisture, volatile matter, fixed carbon, ash) analyses were performed and revealed. The coals herein, as a result of conducted detail prospects and drills, comprises of 0.2 - 1.9 meter thickness, 1.2 % moisture, 30 % ash, 5100 Kcal/kg calorific value and 2.3 million total reserve. The vitrinite (huminite) is the most common maceral and its reflectances (Rmax) were found to be between 0.46 and 1.14% which refer to medium maturity levels. The coals seem to show sub-bituminous to bituminous coal ranks. The mineral matters of the Hazro coals are mostly clays, calcite and pyrite.en_US
dc.description.sponsorshipMinist Environm & Water,Bulgarian Acad Sci,Acad Sci Czech Republ,Acad Sci IR Iran,Latvian Acad Sci,Polish Acad Sci,Russian Acad Sci,Serbian Acad Sci & Arts,Slovak Acad Sci,Natl Acad Sci Ukraine,Bulgarian Ind Assocen_US
dc.description.sponsorship[DUAPK-03-MF-85]; [DUBAP-12-MF-15]en_US
dc.description.sponsorshipThis study was realized within DUAPK-03-MF-85, DUBAP-12-MF-15 project framework. The authors are grateful for Prof. Dr. M. Namik YALCIN (Istanbul University), Velat ALABAS, Kivilcim ONEN, Veysel YALCINDAG (Dicle University) and the coal operation firm owner Faysal KAHRAMAN.en_US
dc.identifier.endpage+en_US
dc.identifier.issn1314-2704
dc.identifier.startpage527en_US
dc.identifier.urihttps://hdl.handle.net/11468/22698
dc.identifier.wosWOS:000348532700068
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.language.isoenen_US
dc.publisherStef92 Technology Ltden_US
dc.relation.ispartof12th International Multidisciplinary Scientific Geoconference, Sgem 2012, Vol. Ii
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectTurkish Coalsen_US
dc.subjectDiyarbakir Hazro Coalsen_US
dc.subjectOrganic Petrography Of Hazro Coalsen_US
dc.subjectPermian Aged Coal Of Turkeyen_US
dc.subjectPaleozoic Coals In Turkeyen_US
dc.titleTHE SECOND PALEOZOIC COAL OF TURKEY, DIYARBAKIR-HAZRO COALS AND THEIR PROPERTIESen_US
dc.titleTHE SECOND PALEOZOIC COAL OF TURKEY, DIYARBAKIR-HAZRO COALS AND THEIR PROPERTIES
dc.typeConference Objecten_US

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