Differential characteristics of large-scale basin evolution and hydrocarbon response of clastic strata in central-western China

Fang Chengming; Huang Zeguang

doi:10.11781/sysydz201606703

Volume 38 Issue 6

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Fang Chengming, Huang Zeguang. Differential characteristics of large-scale basin evolution and hydrocarbon response of clastic strata in central-western China[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(6): 703-712. doi: 10.11781/sysydz201606703

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Fang Chengming, Huang Zeguang. Differential characteristics of large-scale basin evolution and hydrocarbon response of clastic strata in central-western China[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(6): 703-712. doi: 10.11781/sysydz201606703

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Differential characteristics of large-scale basin evolution and hydrocarbon response of clastic strata in central-western China

doi: 10.11781/sysydz201606703

Fang Chengming^1,2,
Huang Zeguang²

1.
School of Earth Resource, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China
2. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

Received Date: 2016-06-17
Rev Recd Date: 2016-09-20
Publish Date: 2016-11-28

Abstract

Abstract

Taking the petroleum accumulation system of clastic strata as the core, and the large-scale basins in the central-western China (Sichuan, Ordos, Junggar and Tarim) as a unified space-time system, we discussed the formation and distribution of accumulation systems and their petroleum response under the control of the superposition of basins since the Late Paleozoic. The formation and distribution of main hydrocarbon source rock strata, self-sourced and self-and-near-sourced petroleum accumulation systems were constrained by the differential structure of prototype compaction during a tectonic transition period. The self-and-far-sourced, externally sourced and hybrid-sourced petroleum accumulation systems were controlled by the tectonic deformation caused by basin superposition. The superposition of intercontinental systems in the Mesozoic to Cenozoic controlled petroleum behavior in different accumulation systems. First, differential tectonic subsidence which generated by foredeep overlap during a tectonic transition period controlled the formation of large lithologic hydrocarbon reservoirs and relative enrichment near tectonic uplift/slope zones in self-and-near-sourced petroleum accumulation systems. Second, the late Yanshanian uplift tilting made the early near-sourcing hydrocarbon reservoirs adjust or dilute. Finally, fault activities ever since the Yanshanian controlled the partial enrichment and high-yielding of hydrocarbon in self-sourced petroleum accumulation systems, and the formation of self-and-far-sourced and externally sourced petroleum accumulation systems. The self-and-near-sourced and self-sourced petroleum accumulations in the Yanshanian uplift or slope are the main hydrocarbon exploration targets in clastic strata in the central basin. In the western basin, we should focus on the externally-sourced and self-and-far-sourced petroleum accumulation systems on the compression-wrench fault belts of active uplifts.
- petroleum accumulation system,
- basin prototype,
- petroleum response,
- clastic strata,
- central-western China

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Differential characteristics of large-scale basin evolution and hydrocarbon response of clastic strata in central-western China

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Differential characteristics of large-scale basin evolution and hydrocarbon response of clastic strata in central-western China

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