冀中坳陷蠡县斜坡古近系沙一下亚段沉积物源分析<sup>*</sup>

doi:10.7605/gdlxb.2016.05.061

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Abstract Based on the testing data,the provenance was determined according to the palaeodrainage pattern and palaeomorphology,clastic components,lithic fragment types,heavy mineral assemblages and ZTR index and seismic profile features. The results show that the sediments of the lower part of Member 1 of Paleogene Shahejie Formation in Lixian Slope mainly derived from the southwestern and northern provenances. The southwestern provenance mainly located in the Taihangshan uplift,whose sediments were carried by the ancient Dashahe river through the southern slope,and the ancient Tanghe river cross Gaoyang low uplift. The northern provenance mainly located in the Niutuozhen low uplift. The southwestern provenance was dominant while the northern one was minor. Xiliu area was a convergence region of both procenances.

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Key words： Lixian Slope Paleogene Shahejie Formation palaeodrainage and palaeomorphology heavy mineral assemblages provenance analysis

Received: 21 March 2016 Published: 01 October 2016

ZTFLH:

P512.2

Fund:; [Co-funded by the National Natural Science Foundation of China(No.41572080.41272132)and Major Science and Technology Research Program of Huabei Oilfield Company,PetroChina(No; HBYT-YJY-2015-JS)]

Corresponding Authors: Liu Jinlong,born in 1992,is a M.S. degree candidate in China University of Geosciences(Beijing). His research field is sedimentology E-mail: 442993143@qq.com.About the corresponding author Li Shengli,born in 1971,doctor,is an associate professor in China University of Geosciences(Beijing). He is mainly engaged in the study of reservoir and sedimentology.E-mail: slli@cugb.edu.cn.

Cite this article:

. Provenance analysis of the lower part of Member 1 of Paleogene Shahejie Formation in Lixian Slope,Central Hebei Depression[J]. JOPC, 2016, 18(5): 809-818.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2016.05.061 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2016/V18/I5/809

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