Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Michael Gardosh"'
The progradation of the Nile River Delta and the thick (~1500m) Sinai-Israel shelf since the Pliocene provide a world class source to sink system feeding a deep (>1.5 km) siliciclastic basin. The general agreement that the Pliocene-to-Recent successi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da95be8fa00d933cc69d0a3e05d81d5a
https://doi.org/10.5194/egusphere-egu2020-3849
https://doi.org/10.5194/egusphere-egu2020-3849
Publikováno v:
Marine and Petroleum Geology. 120:104540
The Pliocene-to-Recent succession in the deep Levant basin is coeval to the development of the Nile River delta and to the progradation of the thick (~1500 m) Sinai-Israel shelf. It hides a series of paleo-channels exhibiting transportation and sedim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::64709bef8f5a3dbab71b86bab7a9ff1c
https://doi.org/10.1016/j.marpetgeo.2020.104540
https://doi.org/10.1016/j.marpetgeo.2020.104540
Publikováno v:
AAPG Bulletin. 95:1763-1793
The Levant margin, in the subsurface of the eastern Mediterranean area, formed during the early Mesozoic following rifting and subsequent opening of the southern Tethys Ocean. This work describes the stratigraphic evolution of the shelf edge and slop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c6854f6d3ba8dc0ec2fa9824ad88ffe3
https://doi.org/10.1306/02081109135
https://doi.org/10.1306/02081109135
Autor:
Grant D. Wach, Hongtao Zhu, Shu Jiang, Tao Jiang, Michael Gardosh, Flávio J. Feijó, Sverre Henriksen, Lorena Moscardelli, Hongliu Zeng, Sudeep Kanungo
Publikováno v:
Interpretation. 6:SOi-SOi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae1bb7e98c83b942415853c213ffe98e
https://doi.org/10.1190/int-2018-0830-spseintro.1
https://doi.org/10.1190/int-2018-0830-spseintro.1
Publikováno v:
Quaternary Research. 38:292-304
The Dead Sea is surrounded by chemical and detrital sediments that were deposited in its larger precursor lakes, Lake Samra and Lake Lisan. The sedimentary history of these lakes was recon-structed by means of 230Th/234U ages of 30 samples, mostly of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::942511c99b6fac6cf5c8aa24c91bc298
https://doi.org/10.1016/0033-5894(92)90039-l
https://doi.org/10.1016/0033-5894(92)90039-l
Autor:
Gian Battista Vai, Mario Grasso, Angelo Camerlenghi, Michael Gardosh, J.M. Woodside, Zvi Ben-Avraham, Emanuele Lodolo
The basins in the Eastern Mediterranean can be divided into those that were formed mainly in post-Miocene time and those that were formed during the rifting episodes that led to the formation of the Neotethys. The younger basins can be further divide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9dada206a982badc04265a415b93c652
http://hdl.handle.net/11585/41493
http://hdl.handle.net/11585/41493