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The Oligocene and Miocene sands in the deep Levant Basin: Provenance and sediment routing

Autor: Adar Glazer, Dov Avigad, Navot Morag, Axel Gerdes

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

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Detrital zircon and rutile U–Pb, Hf isotopes and heavy mineral assemblages of Israeli Miocene sands: Fingerprinting the Arabian provenance of the Levant

Autor: Navot Morag, Axel Gerdes, Avishai Abbo, Dov Avigad

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

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::592370db6b09fd1933bca0e0e6dd237f
https://doi.org/10.1111/bre.12544

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The Cadomian and Variscan record of the Gondwana margin in Israel: Protracted Crustal Evolution between the Arabian-Nubian Shield and multiple Tethyan Oceans

Autor: Avishai Abbo, Dov Avigad, Axel Gerdes, Navot Morag

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

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Detrital zircon evidence for exotic elements in the southern Neotethys: A provenance study of Triassic-Eocene rock units in the Kyrenia terrane, Northern Cyprus

Autor: Adar Glazer, Dov Avigad, Navot Morag, Talip Güngör, Axel Gerdes

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

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The Kyrenia Terrane (Northern Cyprus): Detrital Zircon Evidence for Exotic Elements in the Southern Neotethys

Autor: Axel Gerdes, Navot Morag, A. Glazer, Dov Avigad, Talip Güngör

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

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Drainage response to Arabia-Eurasia collision: Insights from provenance examination of the Cyprian Kythrea flysch (Eastern Mediterranean Basin)

Autor: Uri Shaanan, Navot Morag, Axel Gerdes, Dov Avigad, Talip Güngör

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

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