Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Hatice Ünal Ercan"'
Autor:
Ömer Işık Ece, Hatice Ünal Ercan
Publikováno v:
Minerals, Vol 14, Iss 4, p 353 (2024)
Kaolin-group minerals occur in nature as the result of high-sulfidation acid sulfate, sulfur-poor HCl-, HF- and H2CO3-rich acidic fluid-related hydrothermal alterations and in situ geochemical weathering. These minerals possess different crystallogra
Externí odkaz:
https://doaj.org/article/5c7cc7a0ebde4554a9716001d84c3f9a
Publikováno v:
Clays and Clay Minerals. 70:753-779
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34fb3f013f42c497c4498c0d9c8e190f
https://doi.org/10.1007/s42860-022-00214-4
https://doi.org/10.1007/s42860-022-00214-4
Publikováno v:
International Journal of Earth Sciences.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4182c3d41e4e7f965f954ea35be891fd
https://doi.org/10.1007/s00531-023-02319-0
https://doi.org/10.1007/s00531-023-02319-0
Autor:
İrem Çakır, Cengiz Zabcı, Mehmet Köküm, Hatice Ünal Ercan, Havva Neslihan Kıray, Müge Yazıcı, Mehran Basmenji, Özlem Yağcı, N. Beste Şahinoğlu, Uğur Doğan, Semih Ergintav
The multi-disciplinary studies yield a more complicated picture on seismic cycles, especially with the increasing evidence on creeping, slow slip events, tremors and repeating earthquakes. Recent observations support triggering of large earthquakes e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3638589143f84c4198259b91524a3675
https://doi.org/10.5194/egusphere-egu23-14310
https://doi.org/10.5194/egusphere-egu23-14310
Publikováno v:
SSRN Electronic Journal.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f9e58d449bac9ca43afb841bc3c56637
https://doi.org/10.2139/ssrn.4081105
https://doi.org/10.2139/ssrn.4081105
Publikováno v:
Clays and Clay Minerals. 70:808-808
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8a30040b1e9779ad8df0d4d90789b79
https://doi.org/10.1007/s42860-022-00216-2
https://doi.org/10.1007/s42860-022-00216-2
Publikováno v:
Journal of Geochemical Exploration. 202:1-12
The study area is located in the south of Konya Closed Basin which is the largest Miocene inner basin in Central Anatolia. The aim of this study is to determine the chemical composition of the Miocene halite deposits and depositional environments of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2dad4103ba79e9c6390ed15072b60b2d
https://doi.org/10.1016/j.gexplo.2019.03.004
https://doi.org/10.1016/j.gexplo.2019.03.004
Publikováno v:
Applied Geochemistry. 105:17-30
The Tuz Golu basin located in Central Anatolia contains ancient (Miocene) and recent evaporite deposits. The aim of this study is to determine the origin and evolution of the ancient halite deposits in the basin, particularly whether there is a marin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8f08a5148e5f9f7b8b98243286b3fba
https://doi.org/10.1016/j.apgeochem.2019.04.008
https://doi.org/10.1016/j.apgeochem.2019.04.008
There are many well-known geothermal systems linked to magmatic activity on Earth, many of which eventually express a surface manifestation of the below ground magmatism. The Oligo-Miocene was a period of very active magmatism that took place in West
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b35e13c8cc0878a20b0e8ae136c72792
https://doi.org/10.5194/egusphere-egu21-1496
https://doi.org/10.5194/egusphere-egu21-1496
Publikováno v:
Clays and Clay Minerals. 64:245-274
The Biga Peninsula of NW Turkey is host to many kaolin and halloysite deposits with mineralization occurring at the intersections of fault zones in contact with Late Eocene.Miocene calc-alkaline volcanic rocks. Distinguishing between the relative ove
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ac001cec35ea5a9fd559470642682e9
https://doi.org/10.1346/ccmn.2016.0640305
https://doi.org/10.1346/ccmn.2016.0640305