Cenozoic giant coal-bearing basin belt discovered in China's sea area

Sea area is an important area of oil and gas exploration in China. It has been found that China's sea area mainly consists of coal type oil and gas, and the exploration of coal-bearing series source rocks has become an important part of oil and gas exploration there. Through years of comprehensive geological research in China's sea area, it has been revealed that it has undergone multiple occurrences of tectonic opening and closing movements in varying degrees in the Paleogene, forming 26 Cenozoic sedimentary basins of various types, such as active continental margin, passive continental margin, transitional continental margin and drift rift basins. In the present study, it is observed for the first time that coal type source rocks are mainly developed in 14 continental margin basins in China's sea area, revealing that a very large C-shaped coal-bearing basin group developed there in the Cenozoic. Next, based on the coupling analysis of paleoclimate, paleobotany, paleogeography and paleostructure, it is observed that there are five coal-forming periods in China's sea area, namely the Paleocene, Eocene, early Oligocene, late Oligocene and Miocene-Pliocene, and the coal-forming age is gradually new from north to south. It is also found that the coal seams in the sea area are mainly developed in three coal-forming environments in Cenozoic, namely delta, fan delta and tidal flat-lagoon. The coal seams developed in different environments are characterized by thin thickness, many layers and poor stability. However, the coal-bearing series source rocks in China's sea area have a wide distribution range, very high thickness and large amount, thus forming a material basis for the formation of rich coal type oil and gas.

Automated summary

The sea area in China is an important region for oil and gas exploration, primarily consisting of coal-type hydrocarbons. Coal-bearing source rocks have become a crucial focus in exploration efforts. Comprehensive geological research indicates that the region has undergone numerous tectonic movements, resulting in the formation of 26 Cenozoic sedimentary basins of various types. Recent findings reveal the development of a significant C-shaped coal-bearing basin group in 14 continental margin basins. Analysis based on paleoclimate, paleobotany, paleogeography, and paleostructure suggests the presence of five coal-forming periods, with coal seams mainly developed in three Cenozoic environments. Despite their thinness, multiple layers, and poor stability, the coal-bearing series source rocks in the sea area exhibit a wide distribution range, notable thickness, and significant reserves, providing a material basis for the formation of abundant coal-type oil and gas resources.