Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Navot Morag"'
The Levant Basin in the Eastern Mediterranean contains a ~3 km-thick, predominantly siliciclastic section of Oligocene-Miocene age, which hosts large hydrocarbon reservoirs (“Tamar Sands Play”). A fundamental question raised with respect to this
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::23554b8a22036815509b2ac63cd2fe55
Publikováno v:
Basin Research. 33:1967-1984
[Paleogeographic reconstruction of the Levant area in the Early Miocene (15–20 Ma) highlighting the main sediment routing systems into the deep Levant Basin and their detrital zircon and rutile U‐Pb age spectra and a non metric multi‐dimensiona
The northern extent of the supercontinent Gondwana in the late Neoproterozoic-Cambrian is not well defined. In most localities the continental margin is covered by thick sedimentary successions, formed following the successive rifting of Tethyan Ocea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f132e0ea9b8f43673373ec77f5ce015
https://doi.org/10.5194/egusphere-egu22-1777
https://doi.org/10.5194/egusphere-egu22-1777
Situated between Africa and Eurasia in the eastern Mediterranean, the island of Cyprus has developed on the northern margin of the southern Neotethys by the accretion of three terrains, the Mamonia complex, the Troodos ophiolite, and the Kyrenia terr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::90d115aaa76ebf0b54651ef12c5ccb14
https://doi.org/10.5194/egusphere-egu22-5391
https://doi.org/10.5194/egusphere-egu22-5391
The Kyrenia terrane of northern Cyprus comprises a tectonic stack of Triassic to Eocene rock units interleaved with basic and acid volcanics and minor metamorphic inliers, alongside an Oligocene-Miocene flysch. Our U-Pb-Hf detrital zircon investigati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9906d3f78066038b1aa0c21eb9e0a2d9
https://avesis.deu.edu.tr/publication/details/4465bff7-6c7b-4f60-9383-64a8d9d113de/oai
https://avesis.deu.edu.tr/publication/details/4465bff7-6c7b-4f60-9383-64a8d9d113de/oai
Publikováno v:
Earth and Planetary Science Letters. 516:56-65
The Suez Rift is the northern extension of the Red Sea Rift and is an ideal location to study young continental breakup tectonics. Yet, despite much effort to constrain the timing of rift flank uplift and extensional exhumation in this region, the em
The Cenozoic geodynamics of the north-eastern Mediterranean Basin have been dominated by the subduction of the African Plate under Eurasia. A trench-parallel crustal-scale thrust system (Misis-Kyrenia Thrust System) dissects the southern margin of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22d0ac2d5ba81792e6eca212846e9910
https://avesis.deu.edu.tr/publication/details/23247f69-bb5c-4032-816a-7a7fdb6092a0/oai
https://avesis.deu.edu.tr/publication/details/23247f69-bb5c-4032-816a-7a7fdb6092a0/oai
Autor:
Dario Trombotto, Ronald S. Sletten, Navot Morag, Rivka Amit, Itay Halevy, Amit Mushkin, Alan R. Gillespie, Batbaatar Jigjidsuren
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Goldschmidt2021 abstracts.
Publikováno v:
Journal of Petrology. 61
U–Pb ages, trace element content and oxygen isotope ratios of single zircons from five plagiogranite intrusions of the Troodos ophiolite were measured to determine their crystallization age and assess the importance of fractional crystallization ve