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Characterization and economic potentiality of oil shales in Alquseir and Abutartur Areas , Egypt / Moataz Adel Elshafeiy ; Supervised Ahmed Elkammar , Ahmed Niazy Elbarkooky , Jorn Peckmann

By: Contributor(s): Material type: TextTextLanguage: English Publication details: Cairo : Moataz Adel Elshafeiy , 2012Description: 135P. : charts , facsimiles ; 25cmOther title:
  • توصيف وتقييم إقتصادى للطفلة الزيتية فى منطقتى القصير وأبوطرطور : مصر [Added title page title]
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  • Issued also as CD
Dissertation note: Thesis (Ph.D.) - Cairo University - Faculty of Science - Department of Geology Summary: The upper Cretaceous - Lower Palaeocene black shales of Egypt are part of a giant worldwide belt of organic - rich shales and hosted mainly in the Duwi and Dakhla formations in ascending order . Five main lithofacies are encountered in Abu Tartur section (OSN) and nine in Alquseir section (OSR) . It is worth to mention that organic matter dilutes the REE budget and lowers the chondrite - normalized pattern of the organic - rich sediments relative to their corresponding organic - poor
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Item type Current library Home library Call number Copy number Status Date due Barcode
Thesis Thesis قاعة الرسائل الجامعية - الدور الاول المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.12.15.Ph.D.2012.Mo.C (Browse shelf(Opens below)) Not for loan 01010110058971000
CD - Rom CD - Rom مخـــزن الرســائل الجـــامعية - البدروم المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.12.15.Ph.D.2012.Mo.C (Browse shelf(Opens below)) 58971.CD Not for loan 01020110058971000

Thesis (Ph.D.) - Cairo University - Faculty of Science - Department of Geology

The upper Cretaceous - Lower Palaeocene black shales of Egypt are part of a giant worldwide belt of organic - rich shales and hosted mainly in the Duwi and Dakhla formations in ascending order . Five main lithofacies are encountered in Abu Tartur section (OSN) and nine in Alquseir section (OSR) . It is worth to mention that organic matter dilutes the REE budget and lowers the chondrite - normalized pattern of the organic - rich sediments relative to their corresponding organic - poor

Issued also as CD

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