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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Published in:Revista Colombiana de Biotecnología
Main Authors: Sun, Ke, Tang, Shuheng, Zhang, Songhang, Xi, Zhaodong, Li, Jun
Format: Article in Journal/Newspaper
Language:English
Published: Universidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geociencias 2019
Subjects:
Magma
Thermal activity
Magmatic heating
Water movement channel fracture-crack
Network system
Hierarchical configuration
Actividad térmica
Calefacción magmática
Movimiento de agua en canales de Fractura-grieta
Sistema de red
Configuración jerárquica
Canales
Grieta
Arctic
Online Access:https://revistas.unal.edu.co/index.php/esrj/article/view/78805
id ftuncolombiarev:oai:www.revistas.unal.edu.co:article/78805
record_format openpolar
institution Open Polar
collection Universidad Nacional de Colombia: Portal de Revistas UN
op_collection_id ftuncolombiarev
language English
topic Magma
Thermal activity
Magmatic heating
Water movement channel fracture-crack
Network system
Hierarchical configuration
Actividad térmica
Calefacción magmática
Movimiento de agua en canales de Fractura-grieta
Sistema de red
Configuración jerárquica
spellingShingle Magma
Thermal activity
Magmatic heating
Water movement channel fracture-crack
Network system
Hierarchical configuration
Actividad térmica
Calefacción magmática
Movimiento de agua en canales de Fractura-grieta
Sistema de red
Configuración jerárquica
Sun, Ke
Tang, Shuheng
Zhang, Songhang
Xi, Zhaodong
Li, Jun
The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin
topic_facet Magma
Thermal activity
Magmatic heating
Water movement channel fracture-crack
Network system
Hierarchical configuration
Actividad térmica
Calefacción magmática
Movimiento de agua en canales de Fractura-grieta
Sistema de red
Configuración jerárquica
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. En este estudio, el concepto de mineral metal-no-metal hidrotermal gas-agua se utiliza para analizar los canales de movimiento del agua de calentamiento magmático. También se propone el concepto de configuración jerárquica de las microfisuras fracturas-fallas-grietas de los canales de movimiento del agua de calentamiento magmático. Además, se estudia y analiza el campo térmico de magma formado por el movimiento de agua de calentamiento magmático. Basado en el método de simulación de la cuenca, que se combina con el análisis de la evolución paleotectónica y la restauración de la profundidad de enterramiento en las partes del Medio Oriente de la Cuenca ...
format Article in Journal/Newspaper
author Sun, Ke
Tang, Shuheng
Zhang, Songhang
Xi, Zhaodong
Li, Jun
author_facet Sun, Ke
Tang, Shuheng
Zhang, Songhang
Xi, Zhaodong
Li, Jun
author_sort Sun, Ke
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_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_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_sort magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the qinshui basin
publisher Universidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geociencias
publishDate 2019
url https://revistas.unal.edu.co/index.php/esrj/article/view/78805
long_lat ENVELOPE(-59.693,-59.693,-62.498,-62.498)
ENVELOPE(-45.766,-45.766,-60.616,-60.616)
geographic Canales
Grieta
geographic_facet Canales
Grieta
genre Arctic
genre_facet Arctic
op_source Earth Sciences Research Journal; Vol. 23 No. 1 (2019); 27-34
Earth Sciences Research Journal; Vol. 23 Núm. 1 (2019); 27-34
2339-3459
1794-6190
op_relation https://revistas.unal.edu.co/index.php/esrj/article/view/78805/pdf
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Alalade, B., & Tyson, R. V. (2013). Influence of igneous intrusions on thermal maturity of Late Cretaceous shales in the Tuma well, Chad Basin, NE Nigeria. Journal of African Earth Sciences, 77, 59-66. DOI:10.1016/j.jafrearsci.2012.09.006.
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Frieling, J., Svensen, H. H., Planke, S., Cramwinckel, M. J., Selnes, H., & Sluijs, A. (2016). Thermogenic methane release as a cause for the long duration of the PETM. Proceedings of the National Academy of Sciences of the United States of America, 113(43), 12059-12064. DOI:10.1073/pnas.1603348113.
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Rateau, R., Schofield, N., & Smith, M. (2013). The potential role of igneous intrusions on hydrocarbon migration, West of Shetland. Petroleum Geoscience, 19, 259-272. DOI:10.1144/petgeo2012-035.
Ren, Z., Xiao, H., Liu, L., & Zhang, S. (2005). Determination of Mesozoic tectonic heat event in Qinshui basin. Petroleum Exploration and Development, 32(1), 43-47. DOI:10.3321/j.issn:1000-0747.2005.01.011. (In Chinese)
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https://revistas.unal.edu.co/index.php/esrj/article/view/78805
op_rights Derechos de autor 2019 Earth Sciences Research Journal
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https://doi.org/10.1111/bre.12164
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spelling ftuncolombiarev:oai:www.revistas.unal.edu.co:article/78805 2023-05-15T14:28:30+02:00 The magma thermal field and the shallow-level gas accumulation of tight gas reservoirs in the middle-eastern parts of the Qinshui Basin El campo térmico magma y la acumulación de gas a nivel superficial de reservorios de gas en las partes del Medio Oriente de la Cuenca de Qinshui Sun, Ke Tang, Shuheng Zhang, Songhang Xi, Zhaodong Li, Jun 2019-01-01 application/pdf https://revistas.unal.edu.co/index.php/esrj/article/view/78805 eng eng Universidad Nacional de Colombia - Sede Bogotá - Facultad de Ciencias - Departamento de Geociencias https://revistas.unal.edu.co/index.php/esrj/article/view/78805/pdf Aarnes, I., Planke, S., Trulsvik, M., & Svensen, H. (2015). Contact metamorphism and thermogenic gas generation in the Vøring and Møre basins, offshore Norway, during the Paleocene–Eocene thermal maximum. Journal of the Geological Society, 172(5), 588-598. DOI:10.1144/jgs2014-098. Alalade, B., & Tyson, R. V. (2013). Influence of igneous intrusions on thermal maturity of Late Cretaceous shales in the Tuma well, Chad Basin, NE Nigeria. Journal of African Earth Sciences, 77, 59-66. DOI:10.1016/j.jafrearsci.2012.09.006. Alberdi-Genolet, M., Cavallaro, A., Hernandez, N., Crosta, D. E., & Martinez, L. (2013). Magmatic events and sour crude oils in the Malargüe area of the Neuquén Basin, Argentina. Marine & Petroleum Geology, 43, 48-62. DOI:10.1016/j.marpetgeo.2012.11.005. Blažić, L., & Moreau, J. (2016). Discovery of Lower Cretaceous hydrothermal vent complexes in a late rifting setting, southern North Sea: insights from 3D imaging. Journal of the Geological Society, 174(2), 233-241. DOI:10.1144/jgs2015-155. Cukur, D., Horozal, S., Kim, D. C., Lee, G. H., Han, H. C., & Kang, M. H. (2010). The distribution and characteristics of the igneous complexes in the northern East China Sea Shelf Basin and their implications for hydrocarbon potential. Marine Geophysical Researches, 31(4), 299-313. DOI:10.1007/s11001-010-9112-y. Frieling, J., Svensen, H. H., Planke, S., Cramwinckel, M. J., Selnes, H., & Sluijs, A. (2016). Thermogenic methane release as a cause for the long duration of the PETM. Proceedings of the National Academy of Sciences of the United States of America, 113(43), 12059-12064. DOI:10.1073/pnas.1603348113. Gao, Y., & Liu, L. (2003). Brief introduction of effect of magma intrusion activity on sandstone. Geological Science and Technology Information, 22(2), 13-16. DOI:10.3969/j.issn.1000-7849.2003.02.003. (In Chinese) Hakimi, M. H., Nasher, M. A., Saeed, S. A., Al-Hakame, H., Al-Moliki, T., & Al-Sharabi, K. Q. (2017). Metamorphosis of marine organic matter in the jurassic deposits from Sharab area, Taiz Governorate of southwestern Yemen: Thermal effect of tertiary volcanic rocks. Journal of the Geological Society of India, 89(3), 325-330. DOI:10.1007/s12594-017-0607-x. Iyer, K., Schmid, D. W., Planke, S., & Millett, J. (2017). Modelling hydrothermal venting in volcanic sedimentary basins: Impact on hydrocarbon maturation and paleoclimate. Earth & Planetary Science Letters, 467, 30-42. DOI:10.1016/j.epsl.2017.03.023. Iyer, K., Svensen, H., & Schmid, D. W. (2018). SILLi 1.0: a 1-D numerical tool quantifying the thermal effects of sill intrusions. Geoscientific Model Development, 11(1), 43-60. DOI:10.5194/gmd-11-43-2018. Lee, G. H., Kwon, Y. I., Yoon, C. S., Kim, H. J., & Yoo, H. S. (2006). Igneous complexes in the eastern Northern South Yellow Sea Basin and their implications for hydrocarbon systems. Marine & Petroleum Geology, 23(6):631-645. DOI:10.1016/j.marpetgeo.2006.06.001. Li, J., Li, Z., Qiu, N., Zou, Y., Yu, J., & Liu, J. (2016). Carboniferous-Permian abnormal thermal evolution of the Tarim basin and its implication for deep structure and magmatic activity. Chinese Journal of Geophysics, 59(9), 3318-3329. DOI:10.6038/cjg2016096. (In Chinese) Muirhead, D. K., Bowden, S. A., Parnell, J., & Schofield, N. (2017). Source rock maturation owing to igneous intrusion in rifted margin petroleum systems. Journal of the Geological Society, 174(6), 979-987. DOI:10.1144/jgs2017-011. Peace, A., McCaffrey, K., Imber, J., Hobbs, R., van Hunen, J., & Gerdes, K. (2017). Quantifying the influence of sill intrusion on the thermal evolution of organic‐rich sedimentary rocks in nonvolcanic passive margins: an example from ODP 210‐1276, offshore Newfoundland, Canada. Basin Research, 29(3), 249-265. DOI:10.1111/bre.12131. Polteau, S., Hendriks, B. W. H., Planke, S., Ganerød, M., Corfu, F., Faleide, J. I., . . . Myklebust, R. (2016). The Early Cretaceous Barents Sea Sill Complex: Distribution, 40 Ar/ 39 Ar geochronology, and implications for carbon gas formation. Palaeogeography Palaeoclimatology Palaeoecology. 441(1):83-95. DOI:10.1016/j.palaeo.2015.07.007. Polyansky, O. P., Reverdatto, V. V., Khomenko, A. V., & Kuznetsovab E. N. (2003). Modeling of fluid flow and heat transfer induced by basaltic near-surface magmatism in the Lena-Tunguska petroleum basin (Eastern Siberia, Russia). Journal of Geochemical Exploration, 78-79, 687-692. DOI:10.1016/S0375-6742(03)00079-7. Rateau, R., Schofield, N., & Smith, M. (2013). The potential role of igneous intrusions on hydrocarbon migration, West of Shetland. Petroleum Geoscience, 19, 259-272. DOI:10.1144/petgeo2012-035. Ren, Z., Xiao, H., Liu, L., & Zhang, S. (2005). Determination of Mesozoic tectonic heat event in Qinshui basin. Petroleum Exploration and Development, 32(1), 43-47. DOI:10.3321/j.issn:1000-0747.2005.01.011. (In Chinese) Ren, Z. (2000). Comparison of thermal evolution history in sedimentary basins, north China. Oil & Gas Geology, 21(1), 33-37. DOI:10.3321/j.issn:0253-9985.2000.01.009. (In Chinese) Rodriguez, F., Villar, H., & Baudino, R. (2007). Hydrocarbon Generation, Migration, and Accumulation Related to Igneous Intrusions: An Atypical Petroleum System From the Neuquen Basin of Argentina. SPE-107926-MS. DOI:10.2118/107926-MS. Salmachi, A., Rajabi, M., Reynolds, P., Yarmohammadtooski, Z., & Wainman, C. (2016). The effect of magmatic intrusions on coalbed methane reservoir characteristics: A case study from the Hoskissons coalbed, Gunnedah Basin, Australia. International Journal of Coal Geology, 165, 278-289. DOI:10.1016/j.coal.2016.08.025. Schofield, N., Holford, S., Millett, J., Brown, D., Jolley, D., Passey, S. R., . . . Hole, M. (2017). Regional magma plumbing and emplacement mechanisms of the Faroe‐Shetland Sill Complex: implications for magma transport and petroleum systems within sedimentary basins. Basin Research, 29(1), 41-63. DOI:10.1111/bre.12164. Senger, K., Planke, S., Polteau, S., Ogata, K., & Svensen, H. (2014). Sill emplacement and contact metamorphism in a siliciclastic reservoir on Svalbard, Arctic Norway. Norsk Geologisk Tidsskrift, 94, 155-169. Spacapan, J. B., Palma, J. O., Galland, O., Manceda, R., Rocha, E., & Odorico, A. D. (2018). Thermal impact of igneous sill-complexes on organic-rich formations and implications for petroleum systems: A case study in the northern Neuquén Basin, Argentina. Marine & Petroleum Geology, 91, 519-531. DOI:10.1016/j.marpetgeo.2018.01.018. Sydnes, M., Fjeldskaar, W., Løtveit, I. F., Grunnaleite, I., & Cardozo, N. (2018). The importance of sill thickness and timing of sill emplacement on hydrocarbon maturation. Marine & Petroleum Geology, 89(2), 500-514. DOI:10.1016/j.marpetgeo.2017.10.017. Tian, W., Jiang, Z., Pang, X., Meng, Q., & Gu, L. (2005). Study of the thermal modeling of magma intrusion and its effects on the thermal evolution patterns of source rocks. Journal of Southwest Petroleum Institute, 27(1), 12-16. DOI:10.3863/j.issn.1674-5086.2005.01.004. (In Chinese) Wang, D., & Manga, M. (2015). Organic matter maturation in the contact aureole of an igneous sill as a tracer of hydrothermal convection. Journal of Geophysical Research Solid Earth, 120, 4102-4112. DOI:10.1002/2015JB011877. Wei, S., Shen, Y., & Yang, X. (2017). Assessment of coal measures shale gas reservoir features in Yushe-Wuxiang block, Qinshui basin. Coal Geology of China, 29(8), 25-38. DOI:10.3969/j.issn.1674-1803.2017.08.05. (In Chinese) Witte, J., Bonora, M., Carbone, C., & Oncken, O. (2012). Fracture evolution in oil-producing sills of the Rio Grande Valley, northern Neuquén Basin, Argentina. AAPG Bulletin, 96(7), 1253-1277. DOI:10.1306/10181110152. Xu, H., Fang, L., Zhang, X., Hu, J., & Zhu, H. (2006). Characteristics of early permian magmatic rocks and their impact on hydrocarbon accumulation in tarim basin. Acta Geoscientica Sinica, 27(3), 235-240. DOI:10.3321/j.issn:1006-3021.2006.03.007. (in Chinese) Yuan, J. (1985). Gitology. Beijing: Geological Press. 72-103. (In Chinese) Zanella, A., Cobbold, P. 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DOI:10.1016/j.petrol.2007.05.002. https://revistas.unal.edu.co/index.php/esrj/article/view/78805 Derechos de autor 2019 Earth Sciences Research Journal https://creativecommons.org/licenses/by/4.0 CC-BY Earth Sciences Research Journal; Vol. 23 No. 1 (2019); 27-34 Earth Sciences Research Journal; Vol. 23 Núm. 1 (2019); 27-34 2339-3459 1794-6190 Magma Thermal activity Magmatic heating Water movement channel fracture-crack Network system Hierarchical configuration Actividad térmica Calefacción magmática Movimiento de agua en canales de Fractura-grieta Sistema de red Configuración jerárquica info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftuncolombiarev https://doi.org/10.1016/j.palaeo.2015.07.007 https://doi.org/10.1111/bre.12164 https://doi.org/10.6038/pg20160416 2022-12-14T08:58:05Z 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. En este estudio, el concepto de mineral metal-no-metal hidrotermal gas-agua se utiliza para analizar los canales de movimiento del agua de calentamiento magmático. También se propone el concepto de configuración jerárquica de las microfisuras fracturas-fallas-grietas de los canales de movimiento del agua de calentamiento magmático. Además, se estudia y analiza el campo térmico de magma formado por el movimiento de agua de calentamiento magmático. Basado en el método de simulación de la cuenca, que se combina con el análisis de la evolución paleotectónica y la restauración de la profundidad de enterramiento en las partes del Medio Oriente de la Cuenca ... Article in Journal/Newspaper Arctic Universidad Nacional de Colombia: Portal de Revistas UN Canales ENVELOPE(-59.693,-59.693,-62.498,-62.498) Grieta ENVELOPE(-45.766,-45.766,-60.616,-60.616) Revista Colombiana de Biotecnología 16 2 141 149

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