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المؤلفSadooni, Fadhil N.
المؤلفAl-Saad, Hamad
المؤلفNasir, Sobhi J.
تاريخ الإتاحة2023-11-15T15:25:11Z
تاريخ النشر2004-01-01
اسم المنشورCarbonates and Evaporites
المعرّفhttp://dx.doi.org/10.1007/BF03175193
الاقتباسSadooni, F. N., Al-Saad, H., & Nasir, S. J. (2004). Halul and Sharao islands, offshore Qatar: Remnants of the great Infracambrian Hormuz salt basin. Carbonates and Evaporites, 19, Sadooni, F. N., Al-Saad, H., & Nasir, S. J. (2004). Halul and Sharao islands, offshore Qatar: Remnants of the great Infracambrian Hormuz salt basin. Carbonates and Evaporites, 19, 17-27.‏.‏
الرقم المعياري الدولي للكتاب08912556
معرّف المصادر الموحدhttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=3142534606&origin=inward
معرّف المصادر الموحدhttp://hdl.handle.net/10576/49344
الملخصHalul and Sharao islands, offshore Qatar, are among more than 200 islands in the Gulf region, which are believed to have formed by salt diapirism sourced in the Infracambrian Hormuz Salt Series. The islands are composed of dolomite, anhydrite and igneous materials that were brought to the surface by the rising salt. A model is proposed to explain the presence of relatively undisturbed large slabs of the Hormuz, and the lack of inclusions of any rock materials from the penetrated overlying rocks. It is suggested that whereas the competent overlying rocks are broken and laterally displaced by the salt, the mobile Hormuz suite rocks were transported upward between two pillows of salt.
اللغةen
الناشرspringer link
الموضوعislands
العنوانHalul and Sharao islands, offshore Qatar: Remnants of the great infracambrian Hormuz Salt basin
النوعArticle
الصفحات17-27
رقم العدد1
رقم المجلد19
dc.accessType Abstract Only


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