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dc.contributor.authorLermi A.
dc.contributor.authorSönmez M.
dc.contributor.authorAydin F.
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued2016
dc.identifier.isbn9786197105551 -- 9786197105582 -- 9786197105612 -- 9786197105636 -- 9786197105650 -- 9786197105681
dc.identifier.issn1314-2704
dc.identifier.urihttps://dx.doi.org/10.5593/SGEM2016/B11/S01.053
dc.identifier.urihttps://hdl.handle.net/11480/1880
dc.description16th International Multidisciplinary Scientific GeoConference: Science and Technologies in Geology, Exploration and Mining, SGEM 2016 -- 30 June 2016 through 6 July 2016 -- -- 124231en_US
dc.description.abstractThis paper is to investigate ore-alteration mineralogy and geochemical changes of wall rocks in Kızıltepe Mn mineralization (Çamardı, SE-Niğde), which is located in Ulukışla Basin from the central part of the Turkey. Kızıltepe 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 REE 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 %. © SGEM2016.en_US
dc.language.isoengen_US
dc.publisherInternational Multidisciplinary Scientific Geoconferenceen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectHydrothermal alterationen_US
dc.subjectMass change calculationsen_US
dc.subjectMn mineralizationen_US
dc.subjectTurkeyen_US
dc.subjectÇamardıen_US
dc.titleMineralogy and geochemistry of the Kiziltepe (Çamardi-Niğde) Mn prospect in central Anatolia, Turkeyen_US
dc.typeconferenceObjecten_US
dc.relation.journalInternational Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEMen_US
dc.departmentNiğde ÖHÜen_US
dc.identifier.volume1en_US
dc.identifier.startpage421en_US
dc.identifier.endpage428en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.contributor.institutionauthor[0-Belirlenecek]
dc.identifier.doi10.5593/SGEM2016/B11/S01.053


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