Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Jassim A. Al-Jassim"'
Publikováno v:
Arabian Journal of Geosciences. 10
Eight subsurface sections and a large number of thin sections of the Mishrif Limestone were studied to unravel the depositional facies and environments. The allochems in the Mishrif Formation are dominated by bioclasts, whereas peloids, ooids, and in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::686af658cb8994ff73a8f151757d48d5
https://doi.org/10.1007/s12517-017-2970-8
https://doi.org/10.1007/s12517-017-2970-8
Publikováno v:
Arabian Journal of Geosciences. 6:4771-4783
The depositional facies and environments were unraveling by studying 21 subsurface sections from ten oilfields in the central and southern Iraq and a large number of thin sections of the Nahr Umr (siliciclastic deposit) Formation (Albian). This forma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8bdbf533c206f0cfc67aba20ceeae4f3
https://doi.org/10.1007/s12517-012-0747-7
https://doi.org/10.1007/s12517-012-0747-7
Publikováno v:
Arabian Journal of Geosciences. 6:4743-4754
The Jeribe Formation (Early Middle Miocene) in the central and southern Iraq consists mainly of shallow marine carbonates. Many microfacies have been identified: mudstone, wackestone, packstone, and grainstone with seven submicrofacies. Four major de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3392176b9e51502ab433607b3a4a35ef
https://doi.org/10.1007/s12517-012-0705-4
https://doi.org/10.1007/s12517-012-0705-4
Publikováno v:
Arabian Journal of Geosciences. 3:67-78
Eight subsurface sections and a large number of thin sections of the Mishrif Limestone were studied to unravel the depositional facies and environments. The allochems in the Mishrif Formation are dominated by bioclasts, whereas peloids, ooids, and in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b211a791d22ad51c40d71e952ad6eca1
https://doi.org/10.1007/s12517-009-0057-x
https://doi.org/10.1007/s12517-009-0057-x
Publikováno v:
Sedimentary Geology. 42:279-304
This paper traces the general chrono-petrographic and -petrochemical trends in the evolution of the sand- and silt-sized carbonate clastic beds of the geosynclinal basins bordering the Zagros orogen in north-eastern Iraq. This orogen was repeatedly u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c8c25ca375c19214e6dae8371c77d6f
https://doi.org/10.1016/0037-0738(85)90048-x
https://doi.org/10.1016/0037-0738(85)90048-x
Autor:
Zdenek Kukal, Jassim A. Al-Jassim
Publikováno v:
Sedimentary Geology. 5:57-81
Sedimentological investigations of the lower Bakhtiari Formation in central Iraq proved that this formation represents typical post-orogenic molasse sedimentation. It originated by the rapid erosion of lifted Zagros Mountains and deposition of the co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c565f2da64d5d6e1b2d1e5831ae2ff43
https://doi.org/10.1016/0037-0738(71)90019-4
https://doi.org/10.1016/0037-0738(71)90019-4