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dc.contributor.authorAYSAL, Namık
dc.contributor.authorÖngen, Sinan
dc.contributor.authorHANİLÇİ, Nurullah
dc.contributor.authorKASAPÇI, Cem
dc.contributor.authorLAÇİN, Davut
dc.contributor.authorBoroğlu, Mehtap Şafak
dc.contributor.authorYesiltaş, Mehmet
dc.contributor.authorYILMAZ, İsak
dc.contributor.authorAZAZ, Direnç
dc.date.accessioned2021-03-06T07:51:12Z
dc.date.available2021-03-06T07:51:12Z
dc.identifier.citationAYSAL N., Öngen S., HANİLÇİ N., KASAPÇI C., LAÇİN D., Boroğlu M. Ş. , Yesiltaş M., YILMAZ İ., AZAZ D., "Late magmatic – hydrothermal tourmaline occurrences within leucogranites in NW Anatolia (Turkey): Mineral chemistry and genetic implications", Chemie der Erde, 2020
dc.identifier.issn0009-2819
dc.identifier.othervv_1032021
dc.identifier.otherav_de382a87-6296-4f40-9dfa-8955b438acc5
dc.identifier.urihttp://hdl.handle.net/20.500.12627/146398
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85091927249&origin=inward
dc.identifier.urihttps://doi.org/10.1016/j.chemer.2020.125676
dc.description.abstract© 2020 Elsevier GmbHNumerous Oligo-Miocene plutonic and associated aplite-pegmatite rocks occur in the Western Anatolian Magmatic Complex. However, only the plutons of Namazgah, Karadağ, Soğucak and Karadoru, in the Biga Peninsula, host three different types of tourmaline: disseminated, nodular, and vein-type. These all fall into the alkali subgroup and schorl-oxy-schorl-dravite-oxy-dravite solid solution series. This study shows they were formed during late magmatic to hydrothermal stages in the roof sections (at shallow crustal levels) of the granitoid intrusions. Tourmaline compositions remained fairly homogeneous during the formation and evolution of each stage.
dc.language.isoeng
dc.subjectGeochemistry and Petrology
dc.subjectJeofizik Mühendisliği
dc.subjectJEOKİMYA VE JEOFİZİK
dc.subjectYerbilimleri
dc.subjectTemel Bilimler (SCI)
dc.subjectGeophysics
dc.subjectPhysical Sciences
dc.subjectMühendislik ve Teknoloji
dc.titleLate magmatic – hydrothermal tourmaline occurrences within leucogranites in NW Anatolia (Turkey): Mineral chemistry and genetic implications
dc.typeMakale
dc.relation.journalChemie der Erde
dc.contributor.departmentİstanbul Üniversitesi-Cerrahpaşa , Mühendislik Fakültesi , Jeoloji Mühendisliği Bölümü
dc.contributor.firstauthorID2508213


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