Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Mattash M.[1]"'
Publikováno v:
World Geothermal Congress (WGC) 2020+1, pp. 1–11, Reykjavik, Iceland, April-October 2021
info:cnr-pdr/source/autori:Alnethary M.[1], Sharian A.[1], Mattash M.[1], Minissale A.[2], Alkubati M.[1]/congresso_nome:World Geothermal Congress (WGC) 2020+1/congresso_luogo:Reykjavik, Iceland/congresso_data:April-October 2021/anno:2021/pagina_da:1/pagina_a:11/intervallo_pagine:1–11
info:cnr-pdr/source/autori:Alnethary M.[1], Sharian A.[1], Mattash M.[1], Minissale A.[2], Alkubati M.[1]/congresso_nome:World Geothermal Congress (WGC) 2020+1/congresso_luogo:Reykjavik, Iceland/congresso_data:April-October 2021/anno:2021/pagina_da:1/pagina_a:11/intervallo_pagine:1–11
Yemen has special location in the Middle East with a great geothermal potential because it is located at one of the most active plate boundaries and at the triple junction made up by the Gulf of Aden, Red Sea and African Rift system. This is the key
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::dd3c411ed3e2e07699e6f44312110b2e
https://publications.cnr.it/doc/459117
https://publications.cnr.it/doc/459117
Autor:
Mattash M. [1], Pinarelli L. [2], Vaselli O. [2, Minissale A.[2], Jaimes-Viera M. [4], Al-Kadasi M. [5], Shawki M. [6], Tassi F. [2
Publikováno v:
Arabian journal of geosciences (Internet) (2014). doi:10.1007/s12517-013-1120-1
info:cnr-pdr/source/autori:Mattash M. [1], Pinarelli L. [2], Vaselli O. [2, 3], Minissale A.[2], Jaimes-Viera M. [4], Al-Kadasi M. [5], Shawki M. [6], Tassi F. [2, 3]/titolo:Geochemical evolution of Southern Red Sea and Yemen flood volcanism: evidence for mantle heterogenity./doi:10.1007%2Fs12517-013-1120-1/rivista:Arabian journal of geosciences (Internet)/anno:2014/pagina_da:/pagina_a:/intervallo_pagine:/volume
info:cnr-pdr/source/autori:Mattash M. [1], Pinarelli L. [2], Vaselli O. [2, 3], Minissale A.[2], Jaimes-Viera M. [4], Al-Kadasi M. [5], Shawki M. [6], Tassi F. [2, 3]/titolo:Geochemical evolution of Southern Red Sea and Yemen flood volcanism: evidence for mantle heterogenity./doi:10.1007%2Fs12517-013-1120-1/rivista:Arabian journal of geosciences (Internet)/anno:2014/pagina_da:/pagina_a:/intervallo_pagine:/volume
The Red Sea is part of the Afro-Arabian rift system, the world’s largest active continental rift system. The early opening phases of the Red Sea Rift were accompanied by continental flood magmatism. Large volumes of flood basalts emplaced in the Ol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d732bc6cd9d1afcd1be3b8ea913c88e4
http://link.springer.com/journal/12517
http://link.springer.com/journal/12517
Autor:
Mattash M. [1, Pinarelli L. [3], Vaselli O. [3, Minissale A. [3], Al-Kadasi M. [5], Shawki M. [6], Tassi F. [3
Publikováno v:
International journal of geosciences (Online) 4 (2013): 1459–1466. doi:10.4236/ijg.2013.410143
info:cnr-pdr/source/autori:Mattash M. [1, 2], Pinarelli L. [3], Vaselli O. [3, 4], Minissale A. [3], Al-Kadasi M. [5], Shawki M. [6], Tassi F. [3,4]/titolo:Continental flood basalts and rifting: Geochemistry of cenozoic Yemen volcanic province./doi:10.4236%2Fijg.2013.410143/rivista:International journal of geosciences (Online)/anno:2013/pagina_da:1459/pagina_a:1466/intervallo_pagine:1459–1466/volume:4
info:cnr-pdr/source/autori:Mattash M. [1, 2], Pinarelli L. [3], Vaselli O. [3, 4], Minissale A. [3], Al-Kadasi M. [5], Shawki M. [6], Tassi F. [3,4]/titolo:Continental flood basalts and rifting: Geochemistry of cenozoic Yemen volcanic province./doi:10.4236%2Fijg.2013.410143/rivista:International journal of geosciences (Online)/anno:2013/pagina_da:1459/pagina_a:1466/intervallo_pagine:1459–1466/volume:4
Rift formation is a crucial topic in global tectonics. The Yemen rift-related area is one of the most important provinces, being connected to the rifting processes of the Gulf of Aden, the Red Sea and Afar Triangle. In this paper, a review of the Yem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::35a656d166c4393df6e13e90e7de3c33
http://www.scirp.org/journal/ijg/
http://www.scirp.org/journal/ijg/