Abstract
Organic matter (OM) is the material basis for hydrocarbon generation. Its type and abundance determine the hydrocarbon generation ability of source rocks, which is closely related to the provenance and sedimentary environment of source rocks. The tectonic backgrounds of the eastern and western subsags (ESS and WSS) of the Lishui Sag in the East China Sea Shelf Basin are significantly different and their influence on the OM in the source rocks is worthy of attention. This paper comprehensively analyzes the provenance and environmental characteristics and their influence on the features of the OM of Paleocene source rocks in the ESS and WSS. The study finds that the source rocks in the ESS have multiple sources. During the deposition period, as the salinity and paleoproductivity of the water column increased, the proportion of OM in the autochthonous components of the water column continued to increase, but the overall water column was in an oxidizing environment, resulting in a generally low abundance of OM. The provenance of the source rocks in the WSS was relatively simple and terrestrial. Also, the sedimentary environment had little effect on the type of OM. However, the whole water column of the WSS was in an anoxic environment, so the OM was better preserved, resulting in a higher abundance. Due to the influence of provenance and the sedimentary environment in different areas of the sag, the characteristics of OM in the source rocks are different, so relevant exploration strategies need to be adopted in actual exploration.