2005Zhongguo yanrongRequires access

RESEARCH ON THE CHRON AND ENVIRONMENT OF DIAGENESIS FOR JIANGBEI CONGLOMERATE——Taking the Fuzhong Profile of Beipei,Chongqing as An Example

HE Duo-xing, Shiyou Xie

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Abstract

Jiangbei conglomerate is a kind of supergene cemented rock.Up to now,its diagenetic reasons are not researched deeply and there are different conclusions about the diagenetic reason.The diagenetic chron and environment are studied with~(14)C,ESR and U-Th dating method and δ~(13)C analysis in this paper.It is concluded that the sedimental time of Jiangbei conglomerate was between 10000 and 40000 years,the diagenetic chron was between 10000 and 24300 years.The arid and cold climate during the last stage of late Pleistocene and early Holocene are the major conditions for its diagenesis.

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What this paper is about

Jiangbei conglomerate is a kind of supergene cemented rock.Up to now,its diagenetic reasons are not researched deeply and there are different conclusions about the diagenetic reason.The diagenetic chron and environment are studied with~(14)C,ESR and U-Th dating method and δ~(13)C analysis in this paper.It is concluded that the sedimental time of Jiangbei conglomerate was between 10000 and 40000 years,the diagenetic chron was between 10000 and 24300 years.The arid and cold climate during the last stage of late Pleistocene and early Holocene are the major conditions for its diagenesis.

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Available abstract

Jiangbei conglomerate is a kind of supergene cemented rock.Up to now,its diagenetic reasons are not researched deeply and there are different conclusions about the diagenetic reason.The diagenetic chron and environment are studied with~(14)C,ESR and U-Th dating method and δ~(13)C analysis in this paper.It is concluded that the sedimental time of Jiangbei conglomerate was between 10000 and 40000 years,the diagenetic chron was between 10000 and 24300 years.The arid and cold climate during the last stage of late Pleistocene and early Holocene are the major conditions for its diagenesis.

Key concepts: Diagenesis, Conglomerate, Geology, Geochemistry, Holocene, Paleontology, Sedimentary rock

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