The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin

In this study, the metal-non-metal mineral gas-water hydrothermal concept is used to analyze the movement channels of magmatic heating water. Further, the concept of fractures-faults-cracks microfissures hierarchical configuration of the movement channels of magmatic heating water is proposed. In ad...

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Main Authors: Ke Sun, Shuheng Tang, Songhang Zhang, Zhaodong Xi, Jun Li
Format: Article
Language:English
Published: Universidad Nacional de Colombia 2019-01-01
Series:Earth Sciences Research Journal
Subjects:
Online Access:https://revistas.unal.edu.co/index.php/esrj/article/view/78805
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author Ke Sun
Shuheng Tang
Songhang Zhang
Zhaodong Xi
Jun Li
author_facet Ke Sun
Shuheng Tang
Songhang Zhang
Zhaodong Xi
Jun Li
author_sort Ke Sun
collection DOAJ
description In this study, the metal-non-metal mineral gas-water hydrothermal concept is used to analyze the movement channels of magmatic heating water. Further, the concept of fractures-faults-cracks microfissures hierarchical configuration of the movement channels of magmatic heating water is proposed. In addition, the magma thermal field formed by magmatic heating water movement is studied and analyzed. Based on the basin simulation method, which is combined with the paleo-tectonic evolution analysis and restoration of the ancient burial depth in the middle-eastern parts of the Qinshui Basin, the tectonic evolution history, thermal evolution history, and hydrocarbon generation and exhaustion history of tight gas reservoirs in the Yushe-Wuxiang block in the middle-eastern parts of the Qinshui Basin have been investigated. On the basis of the theories and methods that are proposed in this study, the hierarchical configuration of fractures-faults-cracks microfissures movement channels of magmatic heating water in the Yushe-Wuxiang block in the middle-eastern parts of the Qinshui Basin was studied and analyzed. It is observed that the magmatic heating water rises to the source formation through the movement channels of hierarchical configuration, heats the source rocks, accelerates the evolution of the source rock in the shallow layer, and forms a tight gas reservoir.
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spelling doaj.art-5c49df07b6a442d48214a974dcf1179c2022-12-22T00:07:12ZengUniversidad Nacional de ColombiaEarth Sciences Research Journal1794-61902019-01-01231273410.15446/esrj.v23n1.7880550674The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui BasinKe Sun0Shuheng Tang1Songhang Zhang2Zhaodong Xi3Jun Li4School of Energy resource, China University of Geosciences(Beijing), Beijing, 100083, ChinaSchool of Energy resource, China University of Geosciences(Beijing), Beijing, 100083, ChinaSchool of Energy resource, China University of Geosciences(Beijing), Beijing, 100083, ChinaSchool of Energy resource, China University of Geosciences(Beijing), Beijing, 100083, ChinaCollege of Geoscience and Surveying Engineering, China University of Mining and Technology (Beijing), Beijing, 100083, ChinaIn this study, the metal-non-metal mineral gas-water hydrothermal concept is used to analyze the movement channels of magmatic heating water. Further, the concept of fractures-faults-cracks microfissures hierarchical configuration of the movement channels of magmatic heating water is proposed. In addition, the magma thermal field formed by magmatic heating water movement is studied and analyzed. Based on the basin simulation method, which is combined with the paleo-tectonic evolution analysis and restoration of the ancient burial depth in the middle-eastern parts of the Qinshui Basin, the tectonic evolution history, thermal evolution history, and hydrocarbon generation and exhaustion history of tight gas reservoirs in the Yushe-Wuxiang block in the middle-eastern parts of the Qinshui Basin have been investigated. On the basis of the theories and methods that are proposed in this study, the hierarchical configuration of fractures-faults-cracks microfissures movement channels of magmatic heating water in the Yushe-Wuxiang block in the middle-eastern parts of the Qinshui Basin was studied and analyzed. It is observed that the magmatic heating water rises to the source formation through the movement channels of hierarchical configuration, heats the source rocks, accelerates the evolution of the source rock in the shallow layer, and forms a tight gas reservoir.https://revistas.unal.edu.co/index.php/esrj/article/view/78805magmathermal activitymagmatic heatingwater movement channel fracture-cracknetwork systemhierarchical configuration
spellingShingle Ke Sun
Shuheng Tang
Songhang Zhang
Zhaodong Xi
Jun Li
The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin
Earth Sciences Research Journal
magma
thermal activity
magmatic heating
water movement channel fracture-crack
network system
hierarchical configuration
title The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin
title_full The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin
title_fullStr The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin
title_full_unstemmed The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin
title_short The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin
title_sort magma thermal field and the shallow level gas accumulation of tight gas reservoirs in the middle eastern parts of the qinshui basin
topic magma
thermal activity
magmatic heating
water movement channel fracture-crack
network system
hierarchical configuration
url https://revistas.unal.edu.co/index.php/esrj/article/view/78805
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