Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Şuayip Küpeli"'
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 114, Iss 114, Pp 1-10 (1992)
Bu makalede tanımlanan pirit oluşumları, Attepe demir yatağının (Mansurlu-Feke) doğu bitişiğinde yüzeyleyen infrakambriyen yaşlı birimlerin tabanında yer alırlar. Sözkonusu piritler, iki ayrı mineral parajenezi sunarlar. Bunlardan ilk
Externí odkaz:
https://doaj.org/article/97380787f55f4b41b2e7127704bb92ef
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 121, Iss 121, Pp 18-19 (1999)
Kayseri ili, Yahyalı ilçesinin 28 km güneydoğusunda yer alan inceleme alanında, Üst Kretase yaşlı pelajik çökeller ile ofiyolitik kayaçlar yüzeylemektedir. Bozkır birliğine ait bu birimler, Çavdaruşağı olistostromu ve Pozantı-Fara
Externí odkaz:
https://doaj.org/article/460baf2d40df47f49a2f2fb0628ca8ee
Autor:
Muazzez Çelik Karakaya, Mesut Kirmaci, Mehmet Muzaffer Karadağ, Şuayip Küpeli, Necati Karakaya
Publikováno v:
CLEAN - Soil, Air, Water. 43:27-37
The study area located in the western part of the Eastern Pontides, NE Turkey, represents the eastern part of the metallogenic province of the Black Sea region. The soil, water, and some mosses from the area contain heavy metal pollution from the min
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e4f376144b019cf8d93e2d4cb492974
https://doi.org/10.1002/clen.201200651
https://doi.org/10.1002/clen.201200651
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
Autor:
Şuayip Küpeli
Publikováno v:
Journal of Geochemical Exploration. 105:51-74
Hydrothermal-metasomatic iron ores consisting mainly of siderite, ankerite and hematite are located in the Lower–Middle Cambrian limestone marbles of the Eastern Taurus Belt. The siderite, ankerite, hematite and host rock samples from the deposits
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::956720f053f0cd5d1525120da8868082
https://doi.org/10.1016/j.gexplo.2010.04.001
https://doi.org/10.1016/j.gexplo.2010.04.001
Publikováno v:
Geochemistry. 67:313-322
The Attepe district consists of Precambrian, Lower–Middle Cambrian, Upper Cambrian–Lower Ordovician and Mesozoic formations. It contains several iron deposits and occurrences. Three types of iron-mineralizations can be distinguished in the area;
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5adeb17afd7b6d5a78fe4d69e2e83dfb
https://doi.org/10.1016/j.chemer.2006.01.001
https://doi.org/10.1016/j.chemer.2006.01.001
Publikováno v:
clays and clay minerals. 52:495-509
The Konya region in central Anatolia is covered by Pliocene-Late Pleistocene sediments and volcanites related to the sediments NNW of Karapinar, Turkey. In the area, the Upper Miocene-Quaternary Uzecek Dagi and Karacadag volcanites are generally of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff6a70b60688efb24f109fb36550c484
https://doi.org/10.1346/ccmn.2004.0520410
https://doi.org/10.1346/ccmn.2004.0520410
A number of different types of bentonite deposits formed by hydrothermal alteration and diagenetic processes are to be found in the Ordu area of the Eastern Black Sea region. The Ca- and Na-bentonite deposits are related to Upper Cretaceous tholeitic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::21df31b08be7dc2a5eb5db7610aedf19
https://ddd.uab.cat/record/224732
https://ddd.uab.cat/record/224732
