The Oligocene Yacheng Fm contains the most important source rocks that have been confirmed by exploratory wells in the Qiongdongnan Basin.The efficiency of these source rocks is the key to the breakthrough in natural ...The Oligocene Yacheng Fm contains the most important source rocks that have been confirmed by exploratory wells in the Qiongdongnan Basin.The efficiency of these source rocks is the key to the breakthrough in natural gas exploration in the study area.This paper analyzes the hydrocarbon potential of each sag in this basin from the perspective of control of both source rocks and geothermal heat.Two types of source rocks occur in the Yacheng Fm,namely mudstone of transitional facies and mudstone of neritic facies.Both of them are dominated by a kerogen of type-III,followed by type-II.Their organic matter abundances are controlled by the amount of continental clastic input.The mudstone of transitional facies is commonly higher in organic matter abundance,while that of neritic facies is lower.The coal-measure source rocks of transitional facies were mainly formed in such environments as delta plains,coastal plains and barrier tidal flat-marshes.Due to the control of Cenozoic lithosphere extension and influence of neotectonism,the geothermal gradient,terrestrial heat flow value(HFV)and level of thermal evolution are generally high in deep water.The hot setting not only determines the predominance of gas generation in the deep-water sags,but can promote the shallow-buried source rocks in shallow water into oil window to generate oil.In addition to promoting the hydrocarbon generation of source rocks,the high geothermal and high heat flow value can also speed up the cracking of residual hydrocarbons,thus enhancing hydrocarbon generation efficiency and capacity.According to the theory of joint control of source quality and geothermal heat on hydrocarbon generation,we comprehensively evaluate and rank the exploration potentials of major sags in the Qiongdongnan Basin.These sags are divided into 3 types,of which type-I sags including Yanan,Lingshui,Baodao,Ledong and Huaguang are the highest in hydrocarbon exploration potential.展开更多
基金National Key Basic Research and Development Plan(973 plans)“Basic research on oil and gas formation and distribution in deep water basins in South China Sea”(No.2009CB219400)Special and Significant Project of National Science and Technology“Key technology of marine oil and gas exploration in deep water area”(No.2008ZX05025 and 2011ZX05025)Investigation and Evaluation Project of National Strategic Petroleum Resource Provinces of the Ministry of Land and Resources(No.XQ-2004-05 and XQ-2007-05).
文摘The Oligocene Yacheng Fm contains the most important source rocks that have been confirmed by exploratory wells in the Qiongdongnan Basin.The efficiency of these source rocks is the key to the breakthrough in natural gas exploration in the study area.This paper analyzes the hydrocarbon potential of each sag in this basin from the perspective of control of both source rocks and geothermal heat.Two types of source rocks occur in the Yacheng Fm,namely mudstone of transitional facies and mudstone of neritic facies.Both of them are dominated by a kerogen of type-III,followed by type-II.Their organic matter abundances are controlled by the amount of continental clastic input.The mudstone of transitional facies is commonly higher in organic matter abundance,while that of neritic facies is lower.The coal-measure source rocks of transitional facies were mainly formed in such environments as delta plains,coastal plains and barrier tidal flat-marshes.Due to the control of Cenozoic lithosphere extension and influence of neotectonism,the geothermal gradient,terrestrial heat flow value(HFV)and level of thermal evolution are generally high in deep water.The hot setting not only determines the predominance of gas generation in the deep-water sags,but can promote the shallow-buried source rocks in shallow water into oil window to generate oil.In addition to promoting the hydrocarbon generation of source rocks,the high geothermal and high heat flow value can also speed up the cracking of residual hydrocarbons,thus enhancing hydrocarbon generation efficiency and capacity.According to the theory of joint control of source quality and geothermal heat on hydrocarbon generation,we comprehensively evaluate and rank the exploration potentials of major sags in the Qiongdongnan Basin.These sags are divided into 3 types,of which type-I sags including Yanan,Lingshui,Baodao,Ledong and Huaguang are the highest in hydrocarbon exploration potential.
