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Review of Mesozoic Exploration Plays in the Montenegro – NW Albania Segment of South Adriatic Basin, Zamir Bega and Z. Unlocking Reserves from a Secondary Reservoir in a Mature Field Through Integration and Engineering Approach: A Case Study from Oriente Basin, M-2 Reservoir, Eden-Yuturi Oilfield, Ecuador, Nestor Vasconez, Luciano Bravo, Ricardo Grijalva, Raul Jose Baez, Anne Valdez, Esteban Alba, Diego Tapia, Jonny Lomas, and Martha Castillo, #10978 (2017). Definition, Modes of Occurrence and Pitfalls in Understanding the Term 'Bitumen' in Conventional and Unconventional Petroleum Systems, Andy Pepper, #42111 (2017). High-Resolution Electromagnetic and Gravity Imaging of Wadi Sahba in Central Saudi Arabia, Daniele Colombo, Gary W. Designing and Implementing Applied Geosciences Bachelor and Master Programs Tailored for the Gulf Region, Wilfried Bauer, Michaela Bernecker, Bernhard Heim, Ekkehard Holzbecher, and Wiekert Visser, #70223 (2016).

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A period of extension commenced after ~900 Ma, and in Zambia, the sedimentary sequence began after 880 Ma, with the Lower Roan Subgroup oxidised rift facies clastic rocks, deposited in a series of restricted sub-basins controlled by extensional normal faults, including the thin reduced argillites of the Copperbelt Orebody Member near the middle of the unit.Geological analysis relies mainly on chemistry, physics and mathematics. a'a' lava - basaltic lava characterized by a rough or rubbly surface composed of broken lava blocks called clinker.A-horizon - The uppermost layer of a soil, containing organic material and leached minerals., Naseem Aadil and Ghulam Mohyuddin Sohail, #10364 (2011). World Developments in 2006, (From AAPG Explorer, January 2007), #10120 (2007). Early Permian Siliciclastic System of North-Gondwanaland: A Comparison between Nilawahan Group of North Pakistan and Haushi Group of Oman, Iftikhar Ahmed Abbasi, Muhammad Haneef, and Mohammad Asif Khan, #30227 (2012). Benefiting from Variogram Information to Characterize Facies Distribution in History Matching with En KF, A. Transfer Zones and Hydrocarbon Accumulation in the Albertine Graben of the East African Rift System, Dozith Abeinomugisha and Nurudin Njabire, #10401 (2012). Source Rock Characteristics, Burial History Reconstruction, and Hydrocarbon Generation Modeling of Late Cretaceous Sediments in the Chad (Bornu) Basin, Northeastern Nigeria, Adebanji Kayode Adegoke and Abdullah Wan Hasiah, #10643 (2014).