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Autor:
Pierre Gautier
Publikováno v:
Tectonics. 19:406-409
Autor:
Gautier, Pierre
Publikováno v:
Tectonics; Apr2000, Vol. 19 Issue 2, p406, 4p, 1 Black and White Photograph, 2 Maps
Autor:
Reinhard O. Greiling, Zvi Garfunkel
The geometry and development of foreland basins, being controlled primarily by flexure in front of ad- vancing orogenic wedges, contain information about these causative loads. Modeling of the flexure allows estimating the relations between basin wid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::96fe08d559da974d5cf1799fe3f4d395
https://www.stephan-mueller-spec-publ-ser.net/1/3/2002/smsps-1-3-2002.pdf
https://www.stephan-mueller-spec-publ-ser.net/1/3/2002/smsps-1-3-2002.pdf
Publikováno v:
Journal of African Earth Sciences. 99:332-341
Recently, a detailed (1:50,000) geological map of the Elat area, southern Israel was published. Attached to this map is a stratigraphic table of the Neoproterozoic metamorphic–magmatic complex of the study area. The Neoproterozoic basement in the E
Publikováno v:
Tectonics. 33:166-186
During the past 37 Myr the Levant Basin subsided under a 6 km sedimentary section while the adjacent area, Israel's mountainous backbone (Judea Hills), emerged to an elevation of ~1 km above sea level. What was the flexural contribution of offshore l
Autor:
Hans Friedrichsen, Abraham Starinsky, Zvi Garfunkel, Konrad Hammerschmidt, Adi Torfstein, Yehoshua Kolodny
Publikováno v:
Chemical Geology. 352:188-201
The concentrations and isotopic compositions of helium, and relative abundances of CO2, were studied in brines and freshwater springs, groundwater wells, and gas bubbles, in and around the Dead Sea Transform (DST) fault system. The latter forms part
Publikováno v:
Journal of African Earth Sciences. 68:96-110
The Red Sea is part of a long system of rifts, which formed as a result of African–Arabian continental breakup during the Oligocene–Miocene. Two phases of volcanism are generally accepted, the first occurring 31 mya and the second ∼25 mya. Some
Publikováno v:
Geology. 39:355-358
The recent huge gas discovery in Early Miocene siliciclastics, offshore Israel, highlighted a new world-class gas province, and has subsequently sparked great interest in the Oligocene–Miocene deep-water sediments of the Levant Basin. Based on a de