Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Mazen N. Amaireh"'
Publikováno v:
Journal of African Earth Sciences. 150:701-721
Representative samples from the Al-Hisa Phosphorite Formation (AHP) in the SE desert of Jordan, are selected from three sections: Batn El-Ghoul, Nagb Etayyeg, and Zgaimat Al-Hasah. The samples are investigated geochemically and petrographically. Geoc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2040627e2d40ff9be8cebb6232556122
https://doi.org/10.1016/j.jafrearsci.2018.09.023
https://doi.org/10.1016/j.jafrearsci.2018.09.023
Publikováno v:
Arabian Journal of Geosciences. 11
Three sections from the Al-Hisa Phosphorite Formation (AHP) were measured in the southeastern desert of Jordan: Batn El-Ghoul, Nagb Etayyeg, and Zgaimat Al-Hasah. A fourth section, Wadi Arfa, is added from a previous work. The three sections differ f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ccc6c122423bb218a8f9f7b8e3da5f7
https://doi.org/10.1007/s12517-018-3768-z
https://doi.org/10.1007/s12517-018-3768-z
Autor:
Reyad A. Al Dwairi, Hani Khoury, Osama Y. Shakkoury, Nafeth A. Abdelhadi, Khalid Tarawneh, Mazen N. Amaireh, Hani M. Alnawafleh
Publikováno v:
Open Journal of Geology. :689-700
This work represents the first detailed study of an oil shale (OS) section from the Upper Campanian Amman Silicified Limestone (ASL) Formation in south-western part of Jordan. More than five meters of oil shale have been recorded. Using the petrograp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14a62cb52c4b6f0db80f3a15c8c0161c
https://doi.org/10.4236/ojg.2015.510061
https://doi.org/10.4236/ojg.2015.510061
Tectono sedimentary evolution of the Umm Ghaddah Formation (late Ediacaran-early Cambrian) in Jordan
Publikováno v:
Journal of Asian Earth Sciences. 33:194-218
The terrestrial Umm Ghaddah Formation of late Ediacaran-early Cambrian age was deposited in NE–SW elongated intracontinental rift system basins and sub-basins bounded by active listric half-graben faults. Basin fill consists of conglomerate facies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ad7714be63e26c5d0c30432fe4d7165
https://doi.org/10.1016/j.jseaes.2007.11.003
https://doi.org/10.1016/j.jseaes.2007.11.003