Outcrop characteristic and lithofacies changes of both Gufeng and Dalong Formations in lower Yangtze Region
Vol. 12, Issue 1, Pages: 215-232(2022)
Published:2022
DOI:
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DOI:
YAO Suping, WU Yuyuan, YU Wenduan, et al. Outcrop characteristic and lithofacies changes of both Gufeng and Dalong Formations in lower Yangtze Region[J]. Petroleum Reservoir Evaluation and Development, 2022, 12(1): 215-232.DOI:
Outcrop characteristic and lithofacies changes of both Gufeng and Dalong Formations in lower Yangtze Region
The Middle-Upper Permian Gufeng Formation and Dalong Formation are the important target horizons for the source rock exploration in South China. However
due to the obvious lithologic changes in both spatial and temporal distributions
there is still great controversy in the division and comparison of the regional stratigraphy
which restricts the exploration and potential evaluation of oil and gas resources. Thus here we analyzed six typical field outcrops of the Gufeng and Dalong Formations in the Lower Yangtze regi
on and summarized their lithostratigraphic characteristics. By the regional comparison
we further analyzed their vertical and lateral lithofacies distribution. Combined with the geochemical parameters such as total organic carbon(
TOC
) content
the exploration potential of shale oil and gas is discussed. The results show that the lithological thickness of the Gufeng Formation in the Lower Yangtze region varies greatly
showing the characteristics of alternating thick and thin
and its deposition center is generally located in the areas of Fanchang-Wuhu and Jurong-Lishui. The Gufeng Formation can be basically divided into three members
among which the middle member with interbedded chert and siliceous mudstone is regionally stable and thick. The thickness of the Dalong Formation does not change much regionally
but it is affected by the paleogeographical setting. The lithological differentiation of the Dalong Formation is obvious in the region
and its chert and siliceous mudstone is mainly developed in the southern Anhui area
while in the northern Jiangsu area
it changes to shale. Based on the previous studies
it is suggested that the Gufeng and Dalong Formations of the Lower Yangtze region have high
TOC
contents
good organic matter types
and their maturity is generally within the gas generation range
indicating that they have great shale gas potential. The vertical distribution characteristics of the
TOC
in the Gufeng and Dalong Formations indicate that their middle-upper member is a more favorable horizon for shale gas exploration. Regionally
the Wuwei Basin
Jurong-Nanling Basin
Changzhou-Xuanguang Basin and Wuxi-Suzhou area are the relatively favorable areas for shale gas exploration; the Xuanguang-Meishan Basin and the Jurong Danyang-Huangqiao-Taizhou area have shale oil exploration prospects due to their low maturity.