Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan Basin

The intra-platform of the fourth member of the Dengying Formation in the Upper Sinian of the Sichuan Basin is an important area for gas exploration. To clarify the hydrocarbon accumulation and enrichment patterns and distribution characteristics in this region, a study was conducted on the hydrocarb...

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Main Authors: Yi YANG, Xiang ZHU, Lei ZHANG, Zuxin XU, Lincheng DAI
Format: Article
Language:zho
Published: Editorial Office of Petroleum Geology and Experiment 2025-03-01
Series:Shiyou shiyan dizhi
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Online Access:https://www.sysydz.net/cn/article/doi/10.11781/sysydz2025020384
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author Yi YANG
Xiang ZHU
Lei ZHANG
Zuxin XU
Lincheng DAI
author_facet Yi YANG
Xiang ZHU
Lei ZHANG
Zuxin XU
Lincheng DAI
author_sort Yi YANG
collection DOAJ
description The intra-platform of the fourth member of the Dengying Formation in the Upper Sinian of the Sichuan Basin is an important area for gas exploration. To clarify the hydrocarbon accumulation and enrichment patterns and distribution characteristics in this region, a study was conducted on the hydrocarbon sources and accumulation processes based on geochemical characteristics of natural gas and bitumen, thin-section observation, and fluid inclusion analysis of the intra-platform and platform margin areas. The results indicated that: (1) Compared to the platform margin areas in the fourth member of the Dengying Formation in northern Sichuan Basin, the intra-platform exhibited higher amounts of carbon isotopes in bitumen and natural gas methane and ethane, with smaller amounts of isotopes in hydrogen. This indicated that the oil and gas in the intra-platform mainly originated from a mixed source of the Qiongzhusi Formation and Sinian hydrocarbon source rocks, with a larger contribution from the Sinian source rocks. (2) There were two phases of oil charging and two phases of natural gas charging in the oil and gas reservoirs in the intra-platform of the fourth member of the Dengying Formation in northern Sichuan Basin. The first phase of low-maturity oil charging occurred in the Late Caledonian, the second phase of large-scale crude oil charging took place from the Late Permian to the Middle Triassic, the third phase involved crude oil pyrolysis gas charging during the Middle to Late Jurassic, and the fourth phase was natural gas adjustment charging in the Cretaceous. (3) The Tongnanba area has long been located in the lower part of the paleostructure from the oil accumulation to the gas accumulation period. The crude oil and natural gas from the paleo-oil and gas reservoirs continuously adjusted and migrated towards a higher position in the front of Micang Mountain, resulting in the loss of paleo-gas reservoirs in the Tongnanba area, which now has relatively poor gas content. The Nanjiang area had a more favorable source and reservoir configuration, remaining in the higher part of the paleostructure during the main oil and gas generation periods. It continuously received natural gas charging, and the fault sealing was good, which was conducive to gas reservoir preservation and oil and gas accumulation. Therefore, the Nanjiang area in the intra-platform is the next favorable exploration zone in the fourth member of the Dengying Formation in northern Sichuan Basin.
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publisher Editorial Office of Petroleum Geology and Experiment
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spelling doaj-art-0860de26300d428c90d0b1eee3fbfcdd2025-08-20T02:54:01ZzhoEditorial Office of Petroleum Geology and ExperimentShiyou shiyan dizhi1001-61122025-03-0147238439410.11781/sysydz2025020384sysydz-47-2-384Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan BasinYi YANG0Xiang ZHU1Lei ZHANG2Zuxin XU3Lincheng DAI4State Key Laboratory of Deep Oil and Gas, Chengdu, Sichuan 610041, ChinaState Key Laboratory of Deep Oil and Gas, Chengdu, Sichuan 610041, ChinaState Key Laboratory of Deep Oil and Gas, Chengdu, Sichuan 610041, ChinaState Key Laboratory of Deep Oil and Gas, Chengdu, Sichuan 610041, ChinaState Key Laboratory of Deep Oil and Gas, Chengdu, Sichuan 610041, ChinaThe intra-platform of the fourth member of the Dengying Formation in the Upper Sinian of the Sichuan Basin is an important area for gas exploration. To clarify the hydrocarbon accumulation and enrichment patterns and distribution characteristics in this region, a study was conducted on the hydrocarbon sources and accumulation processes based on geochemical characteristics of natural gas and bitumen, thin-section observation, and fluid inclusion analysis of the intra-platform and platform margin areas. The results indicated that: (1) Compared to the platform margin areas in the fourth member of the Dengying Formation in northern Sichuan Basin, the intra-platform exhibited higher amounts of carbon isotopes in bitumen and natural gas methane and ethane, with smaller amounts of isotopes in hydrogen. This indicated that the oil and gas in the intra-platform mainly originated from a mixed source of the Qiongzhusi Formation and Sinian hydrocarbon source rocks, with a larger contribution from the Sinian source rocks. (2) There were two phases of oil charging and two phases of natural gas charging in the oil and gas reservoirs in the intra-platform of the fourth member of the Dengying Formation in northern Sichuan Basin. The first phase of low-maturity oil charging occurred in the Late Caledonian, the second phase of large-scale crude oil charging took place from the Late Permian to the Middle Triassic, the third phase involved crude oil pyrolysis gas charging during the Middle to Late Jurassic, and the fourth phase was natural gas adjustment charging in the Cretaceous. (3) The Tongnanba area has long been located in the lower part of the paleostructure from the oil accumulation to the gas accumulation period. The crude oil and natural gas from the paleo-oil and gas reservoirs continuously adjusted and migrated towards a higher position in the front of Micang Mountain, resulting in the loss of paleo-gas reservoirs in the Tongnanba area, which now has relatively poor gas content. The Nanjiang area had a more favorable source and reservoir configuration, remaining in the higher part of the paleostructure during the main oil and gas generation periods. It continuously received natural gas charging, and the fault sealing was good, which was conducive to gas reservoir preservation and oil and gas accumulation. Therefore, the Nanjiang area in the intra-platform is the next favorable exploration zone in the fourth member of the Dengying Formation in northern Sichuan Basin.https://www.sysydz.net/cn/article/doi/10.11781/sysydz2025020384hydrocarbon sourcesoil and gas accumulationthe fourth member of dengying formationupper sinianintra-platformnorthern sichuan basin
spellingShingle Yi YANG
Xiang ZHU
Lei ZHANG
Zuxin XU
Lincheng DAI
Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan Basin
Shiyou shiyan dizhi
hydrocarbon sources
oil and gas accumulation
the fourth member of dengying formation
upper sinian
intra-platform
northern sichuan basin
title Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan Basin
title_full Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan Basin
title_fullStr Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan Basin
title_full_unstemmed Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan Basin
title_short Hydrocarbon sources and accumulation processes in intra-platform of the fourth member of Dengying Formation in northern Sichuan Basin
title_sort hydrocarbon sources and accumulation processes in intra platform of the fourth member of dengying formation in northern sichuan basin
topic hydrocarbon sources
oil and gas accumulation
the fourth member of dengying formation
upper sinian
intra-platform
northern sichuan basin
url https://www.sysydz.net/cn/article/doi/10.11781/sysydz2025020384
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