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作 者:Hani M. Alnawafleh Khalid E. Tarawneh Hani N. Khoury Nafeth A. Abdelhadi Osama Y. Shakkoury Reyad A. Dwairi Mazen N. Amaireh
机构地区:[1]Faculty of Engineering, Al-Hussein Bin Talal University, Ma’an, Jordan [2]Faculty of Engineering, Isra University, Amman, Jordan [3]Department of Geology, The University of Jordan, Amman, Jordan [4]Faculty of Engineering Technology, Al Balqa Applied University, Salt, Jordan [5]Natural Resources Authority, Amman, Jordan [6]Faculty of Engineering, Tafila Technical University, Tafila, Jordan
出 处:《Open Journal of Geology》2015年第10期689-700,共12页地质学期刊(英文)
摘 要:This work represents the first detailed study of an oil shale (OS) section from the Upper Campanian Amman Silicified Limestone (ASL) Formation in south-western part of Jordan. More than five meters of oil shale have been recorded. Using the petrography and geochemistry, this study aims to focus on such non-conventional types of oil shale rocks in Jordan and to shed some light on their composition and formational environment. Unlike oil shale from Maastrichtian to early Tertiary, this type of oil shale is highly dolomitized. The dolomite is diagenetic in origin. This oil shale type contains considerable amount of OM and remarkably enriched in some trace elements and shows quite low sulfur content. Results suggest that the formation of dolomite appears to be limited by the rate of organic matter oxidation.This work represents the first detailed study of an oil shale (OS) section from the Upper Campanian Amman Silicified Limestone (ASL) Formation in south-western part of Jordan. More than five meters of oil shale have been recorded. Using the petrography and geochemistry, this study aims to focus on such non-conventional types of oil shale rocks in Jordan and to shed some light on their composition and formational environment. Unlike oil shale from Maastrichtian to early Tertiary, this type of oil shale is highly dolomitized. The dolomite is diagenetic in origin. This oil shale type contains considerable amount of OM and remarkably enriched in some trace elements and shows quite low sulfur content. Results suggest that the formation of dolomite appears to be limited by the rate of organic matter oxidation.
关 键 词:JORDAN Oil SHALE DOLOMITIZATION CAMPANIAN
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