Zobrazeno 1 - 10
of 24
pro vyhledávání: '"Zehra Karakaş"'
Autor:
Zehra Karakaş, Elif Akıska
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 164, Iss 164, Pp 93-117 (2021)
The Sinanpaşa basin, one of the Neogene basins formed in the extensional tectonic regime in Western Anatolia, is located on the eastern margin of Western Anatolia basins containing different types of evaporites, lignite, uranium and clay minerals. M
Externí odkaz:
https://doaj.org/article/957479e770bd4e3ead1e569a2e5152b0
Publikováno v:
Journal of Petroleum Exploration and Production Technology, Vol 9, Iss 1, Pp 141-157 (2018)
Abstract The Neogene Kağızman–Tuzluca Basin is located in the NE Anatolia and extends eastward into Armenia Oktemberian Basin. The Halıkışlak (Late Oligocene), Turabi and Tuzluca formations (Lower–Middle Miocene) are time equivalents of the
Externí odkaz:
https://doaj.org/article/be0129f1f6b04e0f93c984c3b60954ad
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 134, Iss 134, Pp 1-16 (2007)
Mülk-Demirci yöresinde (KD Sivrihisar) yer alan Neojen yaşlı gölsel birimler; kırıntılı-evaporitik çökeller ile volkanik ve piroklastiklerden oluşmaktadır. Miyosen yaşlı volkanik kayaçlar; bazalt ve andezit karakterli lav akmaları; p
Externí odkaz:
https://doaj.org/article/98a33a23e12247cbaaff310640a118d5
Autor:
Selahattin KADİR, Zehra KARAKAŞ
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 122, Iss 122, Pp 43-44 (2000)
Konya'nın güney ve güneybatısında; volkanik, sedimanter ve volkano-sedimanler birimler geniş bir yayılıma sahiptirler. Ignimbirit, kızgın bulut çökelleri ile lav ve domdan oluşan volkanik kayaçlar, mineralojik ve dokusal özelliklerine
Externí odkaz:
https://doaj.org/article/0380173dd51a45a4a3c4314fdd5b5cae
Autor:
Zehra KARAKAŞ, Selahattin KADİR
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 120, Iss 120, Pp 1-2 (1998)
Konya kuzeyinde yer alan Neojen yaşlı gölsel birimler, kireçtaşı, killi kireçtaşı, kiltaşı, çamurtaşı, marn, kumtaşı ve konglomeralardan oluşur, inceleme bölgesinde geniş bir alanda mostra veren kireçtaşlan beyaz-bej-krem renkli,
Externí odkaz:
https://doaj.org/article/ae18bfa81829406090883455df970cdb
Publikováno v:
Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey.
Türkiye’deki manyezit oluşumları, genellikle sedimanter kayaçlar ve altere ultramafik kayaçların kırık ve çatlakları içerisinde damar ve ağsal (stokvörk) şekilde bulunmaktadır. İzmir-Ankara-Erzincan Sütur Kuşağı içerisindeki An
Autor:
Zehra Karakaş
Şeki'de yapılan ilk kilise hakkında genel bilgi vermektedir.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22e2137511caacfb1b6a4188b470e1f1
Autor:
Elif Akiska, Zehra Karakaş
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 164, Iss 164, Pp 93-117 (2021)
Volume: 164, Issue: 164 93-117
Bulletin of the Mineral Research and Exploration
Volume: 164, Issue: 164 93-117
Bulletin of the Mineral Research and Exploration
The Sinanpaşa basin, one of the Neogene basins formed in the extensional tectonic regime in Western Anatolia, is located on the eastern margin of Western Anatolia basins containing different types of evaporites, lignite, uranium and clay minerals. M
Publikováno v:
Journal of Petroleum Exploration and Production Technology, Vol 9, Iss 1, Pp 141-157 (2018)
The Neogene Kağızman–Tuzluca Basin is located in the NE Anatolia and extends eastward into Armenia Oktemberian Basin. The Halıkışlak (Late Oligocene), Turabi and Tuzluca formations (Lower–Middle Miocene) are time equivalents of the organic-r
Publikováno v:
Modern Approaches in Solid Earth Sciences ISBN: 9783030029487
This chapter is about the deposits and the mineral occurrences containing uranium, thorium and rare earth elements in Turkey. The data include exploration studies and the formation/origin and characteristics of these deposits.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a9de85329c7d851af0c07db1cb6811b
https://doi.org/10.1007/978-3-030-02950-0_14
https://doi.org/10.1007/978-3-030-02950-0_14