MINERALOGY AND GEOCHEMISTRY OF THE KIZILTEPE (CAMARDI-NIGDE) MN PROSPECT IN CENTRAL ANATOLIA, TURKEY

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dc.contributor.authorLermi, Abdurrahman
dc.contributor.authorSonmez, Mustafa
dc.contributor.authorAydin, Faruk
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued2016
dc.departmentNiğde ÖHÜ
dc.description16th International Multidisciplinary Scientific Geoconference (SGEM 2016) -- JUN 30-JUL 06, 2016 -- Albena, BULGARIA
dc.description.abstractThis paper is to investigate ore-alteration mineralogy and geochemical changes of wall rocks in Kiziltepe Mn mineralization (Camardi, SE-Nigde), which is located in Ulukisla Basin from the central part of the Turkey. Kiziltepe prospect, a fault controlled hydrothermal-type Mn mineralization, is hosted predominantly by Late Cretaceous to Early Tertiary volcanic and volcanoclastic rock series, which are submarine in character with trachytic to rhyolitic composition. After all samples were systematically collected from surface outcrops and the mineralized zones, they were investigated by petrographical and geochemical analysis. The results obtained from the microscopic and XRD analysis showed that the mineralization contained oxi-hydroxide Mn minerals such as manganite, pyrolusite, psilomelane, and manganese phosphate. Quartz, carbonates, sericite, clay minerals and barite are the gangue minerals. Quartz is ubiquitous and occurs both in the ore zone and in the wall rocks. Alteration mineralogy usually was formed fault-related to alteration zones. Alterations were characterized by presence of quartz and sericite, and locally extensively overprinted by kaolinite. Mass change calculations revealed that Al, Ti, and Y behaved as the least mobile elements during alteration and that footwall felsic rocks gained Fe, Si, K, Ca and ore forming constituents, respectively. The most characteristic chemical changes near the ore bodies were the Na depletion, mainly due to plagioclase destruction by the hydrothermal fluids. The BEE contents varied considerably depending on mass change effects related to alteration. An average grade of Mn in the fault zone has been reached about 22.47 %.
dc.description.sponsorshipBulgarian Acad Sci, Acad Sci Czech Republ, Latvian Acad Sci, Polish Acad Sci, Russian Acad Sci, Serbian Acad Sci & Arts, Slovak Acad Sci, Natl Acad Sci Ukraine, Inst Water Problem & Hydropower NAS KR, Natl Acad Sci Armenia, Sci Council Japan, World Acad Sci, European Acad Sci Arts & Lett, Acad Sci Moldova, Montenegrin Acad Sci & Arts, Croatian Acad Sci & Arts, Georgian Natl Acad Sci, Acad Fine Arts & Design Bratislava, Turkish Acad Sci, Bulgarian Ind Assoc, Bulgarian Minist Environm & Water
dc.description.sponsorshipScientific Research Project Units of the Nigde University [FEB 2006/04]
dc.description.sponsorshipThis study was partly funded by Scientific Research Project Units of the Nigde University under the Project number of FEB 2006/04.
dc.identifier.endpage428
dc.identifier.isbn978-619-7105-55-1
dc.identifier.issn1314-2704
dc.identifier.startpage421
dc.identifier.urihttps://hdl.handle.net/11480/3737
dc.identifier.wosWOS:000393240700053
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.institutionauthor[0-Belirlenecek]
dc.language.isoen
dc.publisherSTEF92 TECHNOLOGY LTD
dc.relation.ispartof16TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE, SGEM 2016: SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING, VOL I
dc.relation.ispartofseriesInternational Multidisciplinary Scientific GeoConference-SGEM
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectCamardi
dc.subjectMn mineralization
dc.subjecthydrothermal alteration
dc.subjectmass change calculations
dc.subjectTurkey
dc.titleMINERALOGY AND GEOCHEMISTRY OF THE KIZILTEPE (CAMARDI-NIGDE) MN PROSPECT IN CENTRAL ANATOLIA, TURKEY
dc.typeConference Object

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