THE GENERATION AND CHARACTERISTICS OF SOURCE ROCKS IN NANPU OIL-RICH DEPRESSION,BOHAI BAY BASIN
Zheng Hong-ju
Abstract
Zheng Hong-ju
Abstract
In recent years,oil-gas exploitation has significant progress and Nanpu depression is found as one of the most oil-rich depressions in Bohai bay Basin.Through the exhaustive research,organic-rich source rocks are identified within Shahejie Formation(Es),especially the TOC(total organic carbon)get the peak abundance in Es34 formation and values commonly exceed 5%.During the early Eocene period when major faulted depression movement occurred,lacustrine basin occupied the largest area and water depth arrived at the highest level in history;wide-spread gray,black mudstone,calcareous mudstone and oil shales prevailed over the stage,which were characteristic of magnificent thickness.The second important hydrocarbon source rocks are fine-grain dark mudstone which develop within Es33 formation.Generally,hydrocarbon source rocks verified in the Es~3_3 member are responsible for the most of hydrocarbon generation that is estimated up to 70%.Although Es_1 member is not comparative with Dongying(Ed) formation in thickness,yet on account of the higher evolution degree,the two source rocks approximately provide nearly 15% oil production separately.
OpenAlex reports 9 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
In recent years,oil-gas exploitation has significant progress and Nanpu depression is found as one of the most oil-rich depressions in Bohai bay Basin.Through the exhaustive research,organic-rich source rocks are identified within Shahejie Formation(Es),especially the TOC(total organic carbon)get the peak abundance in Es34 formation and values commonly exceed 5%.During the early Eocene period when major faulted depression movement occurred,lacustrine basin occupied the largest area and water depth arrived at the highest level in history;wide-spread gray,black mudstone,calcareous mudstone and oil shales prevailed over the stage,which were characteristic of magnificent thickness.The second important hydrocarbon source rocks are fine-grain dark mudstone which develop within Es33 formation.Generally,hydrocarbon source rocks verified in the Es~3_3 member are responsible for the most of hydrocarbon generation that is estimated up to 70%.Although Es_1 member is not comparative with Dongying(Ed) formation in thickness,yet on account of the higher evolution degree,the two source rocks approximately provide nearly 15% oil production separately.
Key concepts: Source rock, Geology, Structural basin, Geochemistry, Bay, Period (music), Total organic carbon, Geomorphology