Hydrocarbon Source Rock Geochemical Characteristics of Xiasiwan Oilfield in the Ordos Basin
Leng Danfeng
Abstract
Leng Danfeng
Abstract
Through its CHANG 4+5,CHANG 6,CHANG 7 layers Department Evaluation of source rocks,CHANG 7 layer of hydrocarbon source rocks is organic carbon content,hydrocarbon generation potential and chloroform bitumen A content of higher,organic matter of typeⅠ1-Ⅱ,good hydrocarbon source rocks.Poor hydrocarbon source rocks and good-medium source rocks of CHANG 6 is quite.Hydrocarbon source rock of CHANG 4 +5 is the non-poor source rocks.Their organic matter are type II2-III.Through the recognization of rock pyrolysis Tmax(℃) and Biomarkers,the layers of source rocks have reached a mature-high mature.
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.
Through its CHANG 4+5,CHANG 6,CHANG 7 layers Department Evaluation of source rocks,CHANG 7 layer of hydrocarbon source rocks is organic carbon content,hydrocarbon generation potential and chloroform bitumen A content of higher,organic matter of typeⅠ1-Ⅱ,good hydrocarbon source rocks.Poor hydrocarbon source rocks and good-medium source rocks of CHANG 6 is quite.Hydrocarbon source rock of CHANG 4 +5 is the non-poor source rocks.Their organic matter are type II2-III.Through the recognization of rock pyrolysis Tmax(℃) and Biomarkers,the layers of source rocks have reached a mature-high mature.
Key concepts: Source rock, Hydrocarbon, Geology, Organic matter, Geochemistry, Pyrolysis, Structural basin, Total organic carbon