Zobrazeno 1 - 10
of 19
pro vyhledávání: '"ERDOĞAN, Tekin"'
Autor:
Aydoğan, Muhammed, Erdoğan, Tekin
This study examined how to utilize emerging technologies to clarify the rights and duties of different components within a given area and create an active control system to overcome complex management problems by using Geographical Information System
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2605::a8faf2bee2b5840e50ba6f55b807041d
https://avesis.deu.edu.tr/publication/details/0b754676-eaac-4191-b7e2-c34f9820ab07/oai
https://avesis.deu.edu.tr/publication/details/0b754676-eaac-4191-b7e2-c34f9820ab07/oai
Publikováno v:
Volume: 27, Issue: 2 127-151
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences
The mollusc faunas from Pliocene deposits of the Hatay-İskenderun region were investigated at nine localities and complemented with three localities from earlier studies. The Pliocene units were deposited in three adjacent subbasins, Hatay-Samandağ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6366de3604ba10c41d5c3941d3ccb8ac
https://doi.org/10.3906/yer-1705-2
https://doi.org/10.3906/yer-1705-2
WOS: 000468485300006
The Hatay Graben (HG), divided into two sub-basins, Hatay-Samandag (HS) and Altinozu-Babatorun (AB) consists of very typical deposits of the pre- and post-evaporite stages spaning to the latest Tortonian/early Messinian to Z
The Hatay Graben (HG), divided into two sub-basins, Hatay-Samandag (HS) and Altinozu-Babatorun (AB) consists of very typical deposits of the pre- and post-evaporite stages spaning to the latest Tortonian/early Messinian to Z
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::87226a65b7791f7b58499ebbead8c65c
https://aperta.ulakbim.gov.tr/record/112104
https://aperta.ulakbim.gov.tr/record/112104
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 117, Iss 117, Pp 1-2 (1995)
Liyas yaşlı Üzümdere formasyonu, bölgedeki paraotokton istifin en yaşlı birimi olup Anamas-Akseki karbonat platformunda yer alır Formasyonu oluşturan litoloji birimleri başta kumtaşlan olmak üzere sırasıyla kireçtaşı, kiltaşı ve ç
Externí odkaz:
https://doaj.org/article/ea29337c634a49f1a525d217e7e6207a
Publikováno v:
Sedimentary Geology. 229:282-298
Messinian evaporites, which resulted from the salinity crisis during the final closure of the Mediterranean Sea, are exposed in SE Turkey. These evaporites formed in two isolated sub-basins, Iskenderun–Arsuz (IA) and Hatay–Samandag (HS), which be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3256195fb3461b7fc69db2b0d5200d3c
https://doi.org/10.1016/j.sedgeo.2010.06.014
https://doi.org/10.1016/j.sedgeo.2010.06.014
Autor:
AKGÜL, ERSİN FIRAT, SOLAK FIŞKIN, Cemile, DÜZALAN, Burak, ERDOĞAN, Tekin, KARATAŞ ÇETİN, ÇİMEN
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2605::c0e42889f399cbb8ac8557d499f6e4c5
https://avesis.deu.edu.tr/publication/details/9f5e509f-f773-4fc5-8a77-6967c7f73df9/oai
https://avesis.deu.edu.tr/publication/details/9f5e509f-f773-4fc5-8a77-6967c7f73df9/oai
Autor:
Erdoğan Tekin
Publikováno v:
Carbonates and Evaporites. 21:33-39
This study reports occurrences of disseminated elemental sulfur in gypsum of the late Miocene Sakarya Formation in Polath-Sivrihisar Basin, located in the Central Anatolia Neogene Basins. Thin-section and scanning-electron microscope studies indicate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::657635cabadd370b6a03f509c8b5ebc5
https://doi.org/10.1007/bf03175466
https://doi.org/10.1007/bf03175466
Publikováno v:
Carbonates and Evaporites. 19:107-117
Jurassic to Lower Cretaceous units, locating Central Taurus composed of thick dolomite with massive limestones beds and thinner dolomite beds with intercalated limestone are described. Various dolomite types include: Type I) dolomite formed as dolomi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2154a8afd7552872952cbae7d1c31276
https://doi.org/10.1007/bf03178474
https://doi.org/10.1007/bf03178474
Publikováno v:
Carbonates and Evaporites. 16:93-101
Celestite-bearing evaporite mineralization is common in the Tertiary evaporitic units of Ulas-Sivas basin, East-Central Turkey.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::072815d49d1970e8ad5eeab148be1ef4
https://doi.org/10.1007/bf03176228
https://doi.org/10.1007/bf03176228
Publikováno v:
Carbonates and Evaporites. 16:1-7
Ooids occurring in the middle Jurassic-lower Cretaceous carbonate sediments of Akseki, Antalya (Turkey) are of two distinct kinds. Type 1 ooids are small and of irregular shape. They have 1 to 4 cortical laminae with a fine radial structure and patch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::969f98cc4e7f0a22db1913d60ab70f9c
https://doi.org/10.1007/bf03176221
https://doi.org/10.1007/bf03176221