深层火成岩侵入体和相关构造发育特征及其石油地质意义——以塔里木盆地顺北地区为例

doi:10.11743/ogg20220109

Abstract

Abstract:

The magma intrusion in the Shunbei area， Tarim Basin， is investigated based on newly acquired 3D seismic data. The igneous intrusions and related structures in the area are characterized and mapped in detail to establish a vertical intrusion model， determine lateral flow direction of magma， and reveal their petroleum significance. The igneous intrusions are saucer-shaped and distribute along the top boundary of the Lower-Middle Ordovician and the boundaries of strata above it in layered superimposition. Reverse faults and steep fractures occur above the saucer-shaped sills， leading to a vertical magma intrusion model of “magma pathway-superimposed sills-steep structure”. The actual distribution of the sills and related structures reveal that the magma in this area fisrt intruded from the deep to the top of the Middle-Lower Ordovician and then flew laterally from north to south in a radial pattern. All these suggest that igneous intrusions play a role in improving reservoir quality and the related reverse faults are the pathways for hydrocarbon to migrate. A deeper understanding of the sills and related structures can be a better guidance for oil and gas exploration in the Shunbei area or even the whole Tarim Basin.

Key words: reverse fault, steep fracture, igneous intrusion, Shunbei area, Tarim Basin

CLC Number:

TE121.2

Yuqing Liu, Shang Deng, Rong Zhang, Jun Liu, Cheng Huang, Tian Gao. Characterization and petroleum geological significance of deep igneous intrusions and related structures in the Shunbei area， Tarim Basin[J]. Oil & Gas Geology, 2022, 43(1): 105-117.

Figures/Tables 13

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Characterization and petroleum geological significance of deep igneous intrusions and related structures in the Shunbei area， Tarim Basin

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