Lower Cretaceous black shales in coastal southeastern China are of significance to the geological study of the Tethys and Pacific realms and to hydrocarbon exploration of southeastern China and East China Sea. However...Lower Cretaceous black shales in coastal southeastern China are of significance to the geological study of the Tethys and Pacific realms and to hydrocarbon exploration of southeastern China and East China Sea. However, the stratigraphic correlation, distribution patterns and hydrocarbon potential of the black shales have not been well constrained so far. In this study, the zircon UePb ages, organic petrologic and geochemical analyses were performed for representative outcrop sections in the region. Zircon UePb ages demonstrate that the Lower Cretaceous black shales in coastal southeastern China can be divided into two regional-scale sets. The first set was deposited during the early stage of the Early Cretaceous（K_1~1, BerriasianeHauterivian）. The second set was deposited during the late stage of the Early Cretaceous（K_1~2）, and might extend to the Taiwan Strait. Detailed organic geochemical analyses including organic matter abundance, type and maturity of the Lower Cretaceous black shales demonstrate that the organic matter abundance of the sources reached medium to good quality by the hydrocarbon source rock standards, and the average TOC values and the chloroform bitumen ＂A＂ of the K_1~1 black shales are higher. The type of organic matter is mainly type III, type II can also be found from the K_1~2 black shales. The thermal maturity of most samples is high to overmature. A relatively comprehensive hydrocarbon resource evaluation indicates that favorable regions are in the northern Guangdong Province for the K_1~1 and in the coastal region of Zhejiang Province and the westernFujian Province for the K_1~2. Sedimentology studies on the Shipu section for the K_1~1 black shales illuminated that the K_1~2 black shales in coastal southeastern China were mainly deposited during transgressive period. The relative sea level changes controlled the sequential development pattern of the K_1~2 black shales.展开更多
基金funded by the National Natural Science Foundation of China (Grant No. 41472099)
文摘Lower Cretaceous black shales in coastal southeastern China are of significance to the geological study of the Tethys and Pacific realms and to hydrocarbon exploration of southeastern China and East China Sea. However, the stratigraphic correlation, distribution patterns and hydrocarbon potential of the black shales have not been well constrained so far. In this study, the zircon UePb ages, organic petrologic and geochemical analyses were performed for representative outcrop sections in the region. Zircon UePb ages demonstrate that the Lower Cretaceous black shales in coastal southeastern China can be divided into two regional-scale sets. The first set was deposited during the early stage of the Early Cretaceous（K_1~1, BerriasianeHauterivian）. The second set was deposited during the late stage of the Early Cretaceous（K_1~2）, and might extend to the Taiwan Strait. Detailed organic geochemical analyses including organic matter abundance, type and maturity of the Lower Cretaceous black shales demonstrate that the organic matter abundance of the sources reached medium to good quality by the hydrocarbon source rock standards, and the average TOC values and the chloroform bitumen ＂A＂ of the K_1~1 black shales are higher. The type of organic matter is mainly type III, type II can also be found from the K_1~2 black shales. The thermal maturity of most samples is high to overmature. A relatively comprehensive hydrocarbon resource evaluation indicates that favorable regions are in the northern Guangdong Province for the K_1~1 and in the coastal region of Zhejiang Province and the westernFujian Province for the K_1~2. Sedimentology studies on the Shipu section for the K_1~1 black shales illuminated that the K_1~2 black shales in coastal southeastern China were mainly deposited during transgressive period. The relative sea level changes controlled the sequential development pattern of the K_1~2 black shales.
