Zobrazeno 1 - 10
of 42
pro vyhledávání: '"Fuat YAVUZ"'
Publikováno v:
Clay Minerals. 52:191-202
This study focused on the mineralogical and physico-chemical properties of heulandite/clinoptilolite (Heu/Cpt)-rich zeolitic tuffs SE of Ankara (Turkey) and evaluated their potential for use as adsorbents. The main Heu/Cpt minerals correspond to the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4339cbcb209226f94886ec08cb5e98e9
https://doi.org/10.1180/claymin.2017.052.2.02
https://doi.org/10.1180/claymin.2017.052.2.02
Publikováno v:
Applied Geochemistry. 124:104830
The kaolin and alunite deposits, situated approximately 20 km southeast of Aksaray in Central Anatolia, were formed by hydrothermal alteration related to extensional tectonics from the Upper Miocene to Quaternary, mostly from rhyolitic volcanoclastic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5003662eea47500be6f342af4737971
https://doi.org/10.1016/j.apgeochem.2020.104830
https://doi.org/10.1016/j.apgeochem.2020.104830
Publikováno v:
Computers & Geosciences. 81:101-113
A Microsoft Visual Basic program, WinCcac, has been developed to calculate the structural formulae of chlorite. WinCcac classifies rock-forming chlorite group minerals based on 14 oxygens for complete chlorite analyses. For electron-microprobe-derive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::807a7aa6e0f8e195b4db880209183d8d
https://doi.org/10.1016/j.cageo.2015.04.011
https://doi.org/10.1016/j.cageo.2015.04.011
Publikováno v:
Clays and Clay Minerals. 63:85-109
The pyroclastic sediments studied here contained varied amounts of zeolite and were formed in the saline alkaline Tuzgolii Basin following the alteration of dacitic volcanic materials during the Early to Late Miocene. The present study focused on the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d421f00f1156b03277fbaee73adfe98f
https://doi.org/10.1346/ccmn.2015.0630202
https://doi.org/10.1346/ccmn.2015.0630202
Publikováno v:
Computers & Geosciences. 63:70-87
A Microsoft Visual Basic program, WinTcac, has been developed to calculate structural formulae of tourmaline analyses based on the Subcommittee on Tourmaline Nomenclature (STN) of the International Mineralogical Association's Commission on New Minera
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::990d622e0a687684e8407b9e8d2b63ed
https://doi.org/10.1016/j.cageo.2013.10.012
https://doi.org/10.1016/j.cageo.2013.10.012
Publikováno v:
Ore Geology Reviews. 56:352-372
In the study region, the Puturge Precambrian–Permian metamorphic rocks, the Upper Jurassic–Lower Cretaceous Guleman ophiolites, the Upper Cretaceous–Lower Eocene Hazar unit, the Campanian–Lower Maastrichtian aged Elazig magmatics, and the Mid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95d722b53a68e8367cfe922e44a3bb0c
https://doi.org/10.1016/j.oregeorev.2013.06.012
https://doi.org/10.1016/j.oregeorev.2013.06.012
Autor:
Fuat Yavuz
Publikováno v:
American Mineralogist. 98:1338-1359
A Microsoft Visual Basic program, called WinPyrox, has been developed to calculate structural formulas of both wet-chemical and microprobe-derived pyroxene analyses. Based on the standard International Mineralogical Association (IMA-88) nomenclature
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::566ae683494649ee1047ee519895dca7
https://doi.org/10.2138/am.2013.4292
https://doi.org/10.2138/am.2013.4292
Publikováno v:
Ore Geology Reviews. 48:197-224
Volcanogenic massive sulfide (VMS) deposits of the Eastern Pontides, Turkey, are hosted by the Maastrichtian–Eocene dacite and rhyodacite series, accompanied by lesser andesite and basalts, as well as their pyroclastic equivalents, with tholeiitic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::028c830900fd4375c7878fe7f1fb4981
https://doi.org/10.1016/j.oregeorev.2012.03.007
https://doi.org/10.1016/j.oregeorev.2012.03.007
Publikováno v:
International Geology Review. 55:158-184
Early Miocene igneous rocks associated with the Dalli porphyry ore body are exposed within the Urumieh-Dokhtar Magmatic Arc (UDMA). The Dalli porphyry Cu–Au deposit is hosted by subduction-related subvolcanic plutons with chemical composition from
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2f1aa9e1a486e68f8412a3f317f95a17
https://doi.org/10.1080/00206814.2012.689640
https://doi.org/10.1080/00206814.2012.689640
Publikováno v:
International Geology Review. 54:1497-1531
The NW–SE-trendingLate Cretaceous–Cenozoic Urumieh-Dokhtar Magmatic Arc (UDMA) in southwest Iran hosts numerous Plio-Quaternary subvolcanic porphyritic andesitic to rhyodacitic domes intruded into a variety of rock sequences. Bulk-rock geochemica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ecc685168b7a80556812a76a069f9ba
https://doi.org/10.1080/00206814.2011.644748
https://doi.org/10.1080/00206814.2011.644748