THE CENOZOIC STRUCTURAL TRANSITION AND ITS SIGNIFICANCE FOR PETROLEUM ACCUMULATION IN DONGYING SAG,SHANDONG
Bin Xia, Cas Key
Abstract
Bin Xia, Cas Key
Abstract
Dongying sag is a secondary structure unit of Jiyang depression, its current structural framework could be regarded as two expanding fault-fold systems controlled by Chennan listric fault zone and Lijin listric fault zone respectively, with each system consisting of four fault-anticline belts. Their evolution history could be divided into three stages as NNE-SSW extension, NW-SE extension and NNE dextral-slipping. This mechanism greatly influenced the process of hydrocarbon generation, migration and accumulation. As a result, structural traps are the most import hydrocarbon preservation units and constitute most of the reservoirs located along the fault-anticline belts.
OpenAlex reports 2 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.
Dongying sag is a secondary structure unit of Jiyang depression, its current structural framework could be regarded as two expanding fault-fold systems controlled by Chennan listric fault zone and Lijin listric fault zone respectively, with each system consisting of four fault-anticline belts. Their evolution history could be divided into three stages as NNE-SSW extension, NW-SE extension and NNE dextral-slipping. This mechanism greatly influenced the process of hydrocarbon generation, migration and accumulation. As a result, structural traps are the most import hydrocarbon preservation units and constitute most of the reservoirs located along the fault-anticline belts.
Key concepts: Anticline, Geology, Fault (geology), Cenozoic, Geochemistry, Petrology, Sinistral and dextral, Geomorphology