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A Review of Carboniferous, Permian and Middle Triassic Paleoenvironmental Linked with Thermal Maturities Interpretation of A1-9 Well, Concession 9, NW Libya

المصدر: المجلة الجامعة
الناشر: جامعة الزاوية - مركز البحوث والدراسات العليا
المؤلف الرئيسي: Alrabib, Mohamed Ali (Author)
مؤلفين آخرين: .Alfandi, Emhemed A (Co-Author) , Fandi, Emad Ibrahim (Co-Author) , Abuharbah, Almagtof Ahmed (Co-Author) , Elyaagubi, Fathi Khalifa (Co-Author)
المجلد/العدد: مج22, ع2
محكمة: نعم
الدولة: ليبيا
التاريخ الميلادي: 2020
الشهر: يونيو
الصفحات: 59 - 82
رقم MD: 1263148
نوع المحتوى: بحوث ومقالات
اللغة: الإنجليزية
قواعد المعلومات: EduSearch, EcoLink, IslamicInfo, AraBase, HumanIndex
مواضيع:
كلمات المؤلف المفتاحية:
Carboniferous | Permian | Middle Triassic | Depositional Paleoenvironmental | Maturity | North Western Libya
رابط المحتوى:
صورة الغلاف QR قانون
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LEADER 02942nam a22003137a 4500
001 2015748
041 |a eng 
044 |b ليبيا 
100 |9 673207  |a Alrabib, Mohamed Ali  |e Author 
245 |a  A Review of Carboniferous, Permian and Middle Triassic Paleoenvironmental Linked with Thermal Maturities Interpretation of A1-9 Well, Concession 9, NW Libya 
260 |b جامعة الزاوية - مركز البحوث والدراسات العليا  |c 2020  |g يونيو 
300 |a 59 - 82 
336 |a بحوث ومقالات  |b Article 
520 |b The present work deals with the paleo environmental and hydrocarbon potential of the lithostratigraphic succession in Carboniferous, Permian and Middle Triassic sediments in the north west Libya. Data presented in this paper are based upon a detailed subsurface lithological characteristics from ditch cutting samples and involving electric logs (gamma-ray) linked with palynofacies interpretation. The sedimentary section of this area ranges in age from Upper Paleozoic rock to Triassic. Early Paleozoic rocks have not been found in the studied well (A1-9), these rocks were eroding during the Late Carboniferous and Early Permian time. During Latest Permian and earliest Triassic time evidence for major marine transgression has occurred. From depths 5930 5940 feet, to 10800-10810 feet, the TAI of the Al Guidr, the Bir Al Jaja Al Uotia, Hebilia and the top varies between 3+ to 4- (mature-dry gas). This interval corporate the rest part of the Dembaba Formation. From depth 10800- 10810 feet, until total sediment depth (11944 feet Log) which corporate the rest of the Dembaba and underlying equivalents of the Assedjefar and M΄rar Formations and the underlying indeterminate unit (Hasaouna Formation), the TAI varies between 4 and 5 (dry gas black & deformed). The environment of deposition and the degree of thermal maturation has allowed the A1-9 well to become a key reference section in NW Libya from which correlations can be carried out. 
653 |a الخصائص الحجرية  |a العصر الكربوني  |a المركبات الكيميائية  |a الهندسة الجيولوجية  |a التضاريس الأرضية  |a ليبيا 
692 |b Carboniferous  |b Permian  |b Middle Triassic  |b Depositional Paleoenvironmental  |b Maturity  |b North Western Libya 
700 |9 673209  |a .Alfandi, Emhemed A  |e Co-Author 
700 |9 673221  |a Fandi, Emad Ibrahim   |e Co-Author 
700 |9 673216  |a Abuharbah, Almagtof Ahmed  |e Co-Author 
700 |9 673213  |a Elyaagubi, Fathi Khalifa  |e Co-Author 
773 |4 العلوم الإنسانية ، متعددة التخصصات  |6 Humanities, Multidisciplinary  |c 008  |e University Bulletin  |l 002  |m مج22, ع2  |o 0928  |s المجلة الجامعة  |v 022 
856 |u 0928-022-002-008.pdf 
930 |d n  |p y  |q n 
995 |a EduSearch 
995 |a EcoLink 
995 |a IslamicInfo 
995 |a AraBase 
995 |a HumanIndex 
999 |c 1263148  |d 1263148