Lithologic Reservoirs ›› 2021, Vol. 33 ›› Issue (4): 1-9.doi: 10.12108/yxyqc.20210401

• PETROLEUM GEOLOGY •     Next Articles

Characteristics and geological significance of Upper Paleozoic paleo-uplift in Fengjie area，Sichuan Basin

YANG Rongjun1,2, PENG Ping3, ZHANG Jing2, YE Mao3, WEN Huaguo4   

  1. 1. PetroChina Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China;
    2. Research Center of Sichuan Basin, PetroChina Research Institute of Petroleum Exploration & Development, Chengdu 610041, China;
    3. Research Institute of Exploration and Development, PetroChina Southwest Oil & Gas Field Company, Chengdu 610041, China;
    4. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
  • Received:2020-08-05 Revised:2020-09-23 Online:2021-08-01 Published:2021-08-06

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Abstract: The stratigraphic structure of Upper Paleozoic in the marginal zone of the eastern Sichuan Basin is complex,and the stratigraphic framework and geological laws are not well understood,especially the limited understanding of the distribution of Carboniferous residual strata and sedimentary facies,which restricts the exploration and development in this zone. Based on the regional geological background,combined with the data of new drilling,new 3D seismic and wild outcrops information,a new understanding that there is a sustained paleo-uplift in Late Paleozoic named Fengjie paleo-uplift in Fengjie-Yunyang area was proposed firstly. In terms of the seismic model forward,the seismic reflection characteristics of Silurian-Devonian-Carboniferous were determined,and the Fengjie paleo-uplift was characterized. By studying the identification,distribution characteristics and tectonic evolution of Carboniferous strata under the control of paleogeomorphology,the analysis of hydrocarbon accumulation conditions of Carboniferous was completed and the favorable gas exploration zone of Carboniferous was predicted and evaluated. The studies suggest that Fengjie paleo-uplift is located about 95 km to the east of Kaijiang paleo-uplift,which is nearly parallel to Kaijiang paleo-uplift. Its overall trend is nearly north-south and slightly east,and the length of north-south axis is about 79 km,however,the width varies from east to west and the average is 14 km in 3D seismic area. Under the joint constraints of Kaijiang paleo-uplift and Fengjie paleo-uplift,the tectonic evolution of the study area can be divided into five stages：Devonian lowstand,Carboniferous lowstand, Carboniferous transgression-highstand,Carboniferous regression and Permian transgression. Because of the longterm continuous evolution of Fengjie paleo-uplift belt,the Carboniferous strata denudation zone can be formed, then with the increase of burial depth,the Carboniferous strata around the paleo-uplift was lateral docking with Silurian mudstone,and the stratigraphic traps would be formed before hydrocarbon charging,even though suffered multiple stages of structural destructions,it may still be preserved as a gas-bearing trap in the present syncline slope area,which can be considered as the foreground area for Carboniferous gas exploration. These understandings provide support for the expansion of Carboniferous gas exploration in eastern Sichuan Basin.

Key words: Carboniferous, Huanglong Formation, stratigraphic-structural composite gas reservoir, Late Paleozoic, Fengjie paleo-uplift, eastern Sichuan Basin

CLC Number: 

  • TE122.3
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