Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Nergis Önalgil"'
Autor:
Tacit Külah, Selahattin Kadir, Nergis Önalgil, Katherine Connell Hewitt, W. Crawford Elliott, Hülya Erkoyun, J. Marion Wampler
Publikováno v:
International Journal of Earth Sciences. 109:2353-2367
Many of the bentonite deposits of the Ankara-cankiri Basin, Central Anatolia, Turkey were found within the Miocene Hancili Formation, which comprises lacustrine sedimentary and volcaniclastic rocks that interfinger with Uludere pyroclastic rocks of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::01447585508ee1d78c3ac89a794441af
https://doi.org/10.1007/s00531-020-01904-x
https://doi.org/10.1007/s00531-020-01904-x
Autor:
Muhsin Eren, Tacit Külah, Selahattin Kadir, Nergis Önalgil Uyanık, Hülya Erkoyun, W. Crawford Elliott
Bentonites have been found widespread within the Bereketli member of the Cretaceous Reşadiye Formation, central Anatolia. These bentonites were hypothesized to have been formed by the in-situ alteration of parent rhyolitic, dacitic, and trachyandesi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4fc9fdc77d916a2a875e79919563a21d
https://hdl.handle.net/20.500.12438/9234
https://hdl.handle.net/20.500.12438/9234
Akademický článek
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Autor:
Tacit Külah, Jennifer Huggett, Muhsin Eren, Hülya Erkoyun, Taner İrkeç, Nergis Önalgil, Selahattin Kadir
Publikováno v:
Clays and Clay Minerals. 65:310-328
WOS: 000423279600002
The Lower Pliocene lacustrine sediments of the Sakarya and Porsuk Formations in the Sivrihisar and Yunusemre-Bicer regions consist of claystone, argillaceous carbonate, carbonate, and evaporites. No detailed studies of paleo
The Lower Pliocene lacustrine sediments of the Sakarya and Porsuk Formations in the Sivrihisar and Yunusemre-Bicer regions consist of claystone, argillaceous carbonate, carbonate, and evaporites. No detailed studies of paleo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d205d77ad62f89e94c72720ed6b017fd
https://doi.org/10.1346/ccmn.2017.064067
https://doi.org/10.1346/ccmn.2017.064067
Publikováno v:
Clays and Clay Minerals. 65:64-91
Widespread alteration in the Miocene lacustrine volcanic/sedimentary rocks of the Ankara-Cankiri basin of central Anatolia has resulted in the formation of sizeable (economic) quantities of bentonite deposits. No detailed characterization of the geol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::436e6b604b7e9ea77ab459f322c377e2
https://doi.org/10.1346/ccmn.2017.064051
https://doi.org/10.1346/ccmn.2017.064051
EUROSOIL Meeting -- OCT 16-21, 2016 -- -- Istanbul, TURKEY
WOS: 000437053000006
Calcretes are common in the Eskisehir province, and occur as powder, nodules, tubes, fracture-infills, and hard laminated crusts. They are white in color, and d
WOS: 000437053000006
Calcretes are common in the Eskisehir province, and occur as powder, nodules, tubes, fracture-infills, and hard laminated crusts. They are white in color, and d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06bb952e5abf99293d87841e548d3ab4
https://hdl.handle.net/20.500.12438/6782
https://hdl.handle.net/20.500.12438/6782
Publikováno v:
Clays and Clay Minerals. 62:267-285
WOS: 000346817200010
The Upper Miocene Mustafapasa member of the Urgup Formation in the Cappadocia region consists predominantly of mudstones, sandstone, and conglomerate lenses with ignimbrite and basalt intercalations. The mudstones are an imp
The Upper Miocene Mustafapasa member of the Urgup Formation in the Cappadocia region consists predominantly of mudstones, sandstone, and conglomerate lenses with ignimbrite and basalt intercalations. The mudstones are an imp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b4866b44bc9c6115e00e1873cc67b5b9
https://doi.org/10.1346/ccmn.2014.0620403
https://doi.org/10.1346/ccmn.2014.0620403
WOS: 000348621500010
Seyfe Lake (Kirsehir, Turkey) is located within a depression zone extending along a NW-SE-trending fault in central Anatolia. Evaporite and carbonate sediments occur at the bottom of the lake which is fed by high-sulfate spr
Seyfe Lake (Kirsehir, Turkey) is located within a depression zone extending along a NW-SE-trending fault in central Anatolia. Evaporite and carbonate sediments occur at the bottom of the lake which is fed by high-sulfate spr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5731df06c972671f1f64c93cb0c8937e
https://hdl.handle.net/11480/3980
https://hdl.handle.net/11480/3980
WOS: 000342659400009
This paper addresses the mineralogy, geochemistry, and genesis of palygorskite and associated calcretes in the Kirsehir region. In this area, the Quaternary calcretes are present within and/or on lacustrine mudstones of the
This paper addresses the mineralogy, geochemistry, and genesis of palygorskite and associated calcretes in the Kirsehir region. In this area, the Quaternary calcretes are present within and/or on lacustrine mudstones of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f367e0ec7b6e784b03a3046fdcad628d
https://hdl.handle.net/11480/4161
https://hdl.handle.net/11480/4161