Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Hilmy E. MOUSSA"'
Autor:
Mohamed W. Ali-Bik, Safwat S. Gabr, Hilmy E. Moussa, Doris Sadek Ghabrial, Said H. Abd El Rahim
Publikováno v:
Egyptian Journal of Remote Sensing and Space Sciences, Vol 25, Iss 2, Pp 445-461 (2022)
Sinai Mesozoic basalts are restricted in its southwestern portion at Um Bogma area, where they occur as intra-continental fissure-fed sills, dykes, plugs and lava flows, following mainly the older structural and crustal weaknesses planes. During Late
Externí odkaz:
https://doaj.org/article/e5a32426405a44c1be683cc761da8e9e
Publikováno v:
Acta Geologica Sinica - English Edition. 96:1545-1565
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25a8b13e14f84b5307d5114b958b1d3b
https://doi.org/10.1111/1755-6724.14915
https://doi.org/10.1111/1755-6724.14915
Autor:
Hilmy E. Moussa, Heba S. Mubarak, Mokhles K. Azer, Adel A. Surour, Paul D. Asimow, Mona M.L. Kabesh
Podiform chromitites are found in the mantle sections of ophiolites in many places and times in the geologic record. Leading theories for their origin invoke melt-rock reaction processes involving hydrous melts in supra-subduction zone settings. Here
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7c938a09b2722e701dcf705f4df44ffc
https://resolver.caltech.edu/CaltechAUTHORS:20220104-157910000
https://resolver.caltech.edu/CaltechAUTHORS:20220104-157910000
Autor:
Hilmy E. Moussa, Paul D. Asimow, Heba S. Mubarak, Adel A. Surour, Mokhles K. Azer, Mona M. L. Kabesh
We studied rodingite and rodingite-like rocks within a serpentinized ultramafic sequence and ophiolitic melange at Um Rashid, in the Eastern Desert of Egypt. The Um Rashid ophiolite is strongly deformed, metamorphosed, and altered by serpentinization
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac1f31ddd050e2f2c397c956c2ac942c
https://resolver.caltech.edu/CaltechAUTHORS:20200812-083037133
https://resolver.caltech.edu/CaltechAUTHORS:20200812-083037133
Autor:
Mokhles K. Azer, Nagy N. Yanni, Mustafa A. Elsagheer, Hilmy E. Moussa, Ayman E. Maurice, Adel I.M. Akarish, Moustafa A. Abou El Maaty, Ahmed A. Elnazer
Publikováno v:
Lithos. :106525
The ultramafic rocks of Gabal Balamhindit are exposed as conspicuous ridges in the south Eastern Desert of Egypt, Northern Nubian Shield. These rocks include extensively to completely serpentinized harzburgites and dunites, which are listvenitized al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1034654159a452eaa966d9c1fb2f4454
https://doi.org/10.1016/j.lithos.2021.106525
https://doi.org/10.1016/j.lithos.2021.106525
Autor:
Nagy N. Yanni, Mokhles K. Azer, M.J. Wilner, Hilmy E. Moussa, Mustafa A. Elsagheer, Adel I.M. Akarish, Heba S. Mubarak, Moustafa A. Abou El Maaty, Paul D. Asimow
Publikováno v:
Lithos. :106405
The Nuweibi intrusion was emplaced during the final tectono-magmatic stage of Arabian-Nubian Shield development (ANS). Two cogenetic phases of intrusion can be recognized in the field: the early phase is represented by porphyritic albite granite and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::592501a66beb289c7ae8f925eaaec0f4
https://doi.org/10.1016/j.lithos.2021.106405
https://doi.org/10.1016/j.lithos.2021.106405
Autor:
Kamal A. Ali, Robert J. Stern, Minghua Ren, M.D. Samuel, Mokhles K. Azer, H. A. Gahlan, Hilmy E. Moussa
Publikováno v:
Mineralogy and Petrology. 107:829-848
The Wadi Allaqi ophiolite along the Egyptian-Sudanese border defines the southernmost ophiolitic assemblage and suture zone in the Eastern Desert. Ophiolite assemblages comprise nappes composed mainly of mafic and ultramafic rocks that were tectonica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebb3cf4f259fd4a386d32f3f36e5f3b8
https://doi.org/10.1007/s00710-012-0204-z
https://doi.org/10.1007/s00710-012-0204-z
Autor:
Hilmy E. Moussa, Martin J. Whitehouse, Yaron Be'eri-Shlevin, Mekhaiel D. Samuel, Mokhles K. Azer
Publikováno v:
Gondwana Research. 20:450-464
The volcano-sedimentary succession at Wadi Rutig, Sinai, at the northernmost segment of the Arabian Nubian Shield comprises early Ediacaran volcanic rocks interbedded with immature sediments including variable sized conglomerates, sandstones and silt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::461489c7a7bd50befa739fc53872e6d9
https://doi.org/10.1016/j.gr.2010.11.021
https://doi.org/10.1016/j.gr.2010.11.021
Autor:
Martin J. Whitehouse, Hilmy E. Moussa, Mokhles K. Azer, M.D. Samuel, Yaron Be'eri-Shlevin, Osmo Tapani Rämö
Publikováno v:
Precambrian Research. 188:21-44
Late Neoproterozoic (Ediacaran) evolution of the northernmost segment of the Arabian-Nubian Shield (ANS) included vast intrusion of granitoids and development of volcano-sedimentary basins. Here we describe two of such volcano-sedimentary successions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81f4b5bac716c271feccf2c921228dd2
https://doi.org/10.1016/j.precamres.2011.04.002
https://doi.org/10.1016/j.precamres.2011.04.002