Zobrazeno 1 - 10
of 137
pro vyhledávání: '"Y. Harlavan"'
Publikováno v:
The Cryosphere, Vol 17, Pp 3363-3381 (2023)
Deglaciation in Svalbard was followed by seawater ingression and deposition of marine (deltaic) sediments in fjord valleys, while elastic rebound resulted in fast land uplift and the exposure of these sediments to the atmosphere, whereby the formatio
Externí odkaz:
https://doaj.org/article/539816a81a9d47ca94fe98012a9d2688
Autor:
Kevin G. Brown, I. Levkov, Y. Harlavan, Jiwchar Ganor, C. Gruber, Ofra Klein-BenDavid, N. Teutsch
Publikováno v:
Science of The Total Environment. 689:469-480
Deep geological repository is considered the internationally accepted method for spent fuel (SF) disposal. In countries where salt, clay, tuff and granite are unavailable at geologically suitable area, other rock types may come into consideration. In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3f070768a915f1898a59940f48eb57fc
https://doi.org/10.1016/j.scitotenv.2019.06.396
https://doi.org/10.1016/j.scitotenv.2019.06.396
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Publikováno v:
Journal of Structural Geology. 77:11-26
We resolve the anisotropy of magnetic susceptibility (AMS) axes along fault planes, cores and damage zones in rocks that crop out next to the Dead Sea Transform (DST) plate boundary. We measured 261 samples of mainly diamagnetic dolostones that were
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88dd87d235576f2a6e914a6acc62264f
https://doi.org/10.1016/j.jsg.2015.05.007
https://doi.org/10.1016/j.jsg.2015.05.007
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
A. Sandler, Y. Harlavan
Publikováno v:
Sedimentary Geology. 229:254-267
Authigenic sedimentary low-temperature K-feldspar separated from Albian–Turonian carbonates in Israel was dated by the step-heating 40Ar–39Ar method. In contrast to high-temperature K-feldspars, ca. 90% of the radiogenic Ar was released at temper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e77ff46d6ee08f780c0311e5db30f72
https://doi.org/10.1016/j.sedgeo.2010.06.012
https://doi.org/10.1016/j.sedgeo.2010.06.012
Publikováno v:
Geological Journal. 44:79-103
The Ilica, Cataldag and Kozak granitoids, cropping out in the northern part of the Izmir-Ankara (IA) suture zone in west Anatolia, Turkey, intrude metamorphic rocks of the Sakarya continent (SC) and Karakaya complex, and are unconformably overlain by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::48f18c001bca21c81cd49e4432d9aa26
https://doi.org/10.1002/gj.1132
https://doi.org/10.1002/gj.1132
Autor:
Y. Harlavan, A. Sandler
Publikováno v:
Clay Minerals. 41:637-658
Clay and glauconite fractions separated from sedimentary rocks in Israel were analysed for their mineralogical composition by X-ray diffraction and dated by the K-Ar method. The main goal was to evaluate early diagenetic processes which might have af
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::091b9e5193a9d8de6fc6afd1495f74cb
https://doi.org/10.1180/0009855064120210
https://doi.org/10.1180/0009855064120210
Autor:
Matthew T. Heizler, Lothar Ratschbacher, Durmuş Boztuğ, Raymond Jonckheere, M. Tichomirova, Y. Harlavan
WOS: 000268847200014
The Middle to Late Cretaceous central Anatolian granitoids intrude the supra-subduction zone-type central Anatolian ophiolite and medium- to high-grade metasediments of central Anatolian crystalline complex and are overlain
The Middle to Late Cretaceous central Anatolian granitoids intrude the supra-subduction zone-type central Anatolian ophiolite and medium- to high-grade metasediments of central Anatolian crystalline complex and are overlain
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1fd4954a198b5364698be619dcf40e6a
https://aperta.ulakbim.gov.tr/record/41609
https://aperta.ulakbim.gov.tr/record/41609
Publikováno v:
Mineralogy and Petrology
Mineralogy and Petrology, Springer Verlag, 2007, 91, pp.191-223
Mineralogy and Petrology, Springer Verlag, 2007, 91, pp.191-223
WOS: 000250593500003
The composite Yozgat batholith consists of a S-I-A-type granitoid association intruding the supra-subduction zone-type (SSZ-type) central Anatolian ophiolite and medium-to high-grade metasedimentary rocks of the central Anat
The composite Yozgat batholith consists of a S-I-A-type granitoid association intruding the supra-subduction zone-type (SSZ-type) central Anatolian ophiolite and medium-to high-grade metasedimentary rocks of the central Anat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40e7071b21ef8b690f922b992cbce225
https://hal.science/hal-00268844
https://hal.science/hal-00268844