Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system

The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Hanping Wan [verfasserIn] Qiao Wang [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	magnetotelluric audio magnetotelluric Gulu geothermal filed geothermal system model electrical structure

Übergeordnetes Werk:	In: Frontiers in Earth Science - Frontiers Media S.A., 2014, 11(2023)
Übergeordnetes Werk:	volume:11 ; year:2023

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3389/feart.2023.1138360

Katalog-ID:	DOAJ08309220X

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allfields	10.3389/feart.2023.1138360 doi (DE-627)DOAJ08309220X (DE-599)DOAJ5b04e8703f8a43f0b1b9f8478db9c61f DE-627 ger DE-627 rakwb eng Hanping Wan verfasserin aut Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs. magnetotelluric audio magnetotelluric Gulu geothermal filed geothermal system model electrical structure Science Q Qiao Wang verfasserin aut In Frontiers in Earth Science Frontiers Media S.A., 2014 11(2023) (DE-627)771399731 (DE-600)2741235-0 22966463 nnns volume:11 year:2023 https://doi.org/10.3389/feart.2023.1138360 kostenfrei https://doaj.org/article/5b04e8703f8a43f0b1b9f8478db9c61f kostenfrei https://www.frontiersin.org/articles/10.3389/feart.2023.1138360/full kostenfrei https://doaj.org/toc/2296-6463 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2023
spelling	10.3389/feart.2023.1138360 doi (DE-627)DOAJ08309220X (DE-599)DOAJ5b04e8703f8a43f0b1b9f8478db9c61f DE-627 ger DE-627 rakwb eng Hanping Wan verfasserin aut Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs. magnetotelluric audio magnetotelluric Gulu geothermal filed geothermal system model electrical structure Science Q Qiao Wang verfasserin aut In Frontiers in Earth Science Frontiers Media S.A., 2014 11(2023) (DE-627)771399731 (DE-600)2741235-0 22966463 nnns volume:11 year:2023 https://doi.org/10.3389/feart.2023.1138360 kostenfrei https://doaj.org/article/5b04e8703f8a43f0b1b9f8478db9c61f kostenfrei https://www.frontiersin.org/articles/10.3389/feart.2023.1138360/full kostenfrei https://doaj.org/toc/2296-6463 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2023
allfields_unstemmed	10.3389/feart.2023.1138360 doi (DE-627)DOAJ08309220X (DE-599)DOAJ5b04e8703f8a43f0b1b9f8478db9c61f DE-627 ger DE-627 rakwb eng Hanping Wan verfasserin aut Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs. magnetotelluric audio magnetotelluric Gulu geothermal filed geothermal system model electrical structure Science Q Qiao Wang verfasserin aut In Frontiers in Earth Science Frontiers Media S.A., 2014 11(2023) (DE-627)771399731 (DE-600)2741235-0 22966463 nnns volume:11 year:2023 https://doi.org/10.3389/feart.2023.1138360 kostenfrei https://doaj.org/article/5b04e8703f8a43f0b1b9f8478db9c61f kostenfrei https://www.frontiersin.org/articles/10.3389/feart.2023.1138360/full kostenfrei https://doaj.org/toc/2296-6463 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2023
allfieldsGer	10.3389/feart.2023.1138360 doi (DE-627)DOAJ08309220X (DE-599)DOAJ5b04e8703f8a43f0b1b9f8478db9c61f DE-627 ger DE-627 rakwb eng Hanping Wan verfasserin aut Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs. magnetotelluric audio magnetotelluric Gulu geothermal filed geothermal system model electrical structure Science Q Qiao Wang verfasserin aut In Frontiers in Earth Science Frontiers Media S.A., 2014 11(2023) (DE-627)771399731 (DE-600)2741235-0 22966463 nnns volume:11 year:2023 https://doi.org/10.3389/feart.2023.1138360 kostenfrei https://doaj.org/article/5b04e8703f8a43f0b1b9f8478db9c61f kostenfrei https://www.frontiersin.org/articles/10.3389/feart.2023.1138360/full kostenfrei https://doaj.org/toc/2296-6463 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2023
allfieldsSound	10.3389/feart.2023.1138360 doi (DE-627)DOAJ08309220X (DE-599)DOAJ5b04e8703f8a43f0b1b9f8478db9c61f DE-627 ger DE-627 rakwb eng Hanping Wan verfasserin aut Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs. magnetotelluric audio magnetotelluric Gulu geothermal filed geothermal system model electrical structure Science Q Qiao Wang verfasserin aut In Frontiers in Earth Science Frontiers Media S.A., 2014 11(2023) (DE-627)771399731 (DE-600)2741235-0 22966463 nnns volume:11 year:2023 https://doi.org/10.3389/feart.2023.1138360 kostenfrei https://doaj.org/article/5b04e8703f8a43f0b1b9f8478db9c61f kostenfrei https://www.frontiersin.org/articles/10.3389/feart.2023.1138360/full kostenfrei https://doaj.org/toc/2296-6463 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 11 2023
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authorswithroles_txt_mv	Hanping Wan @@aut@@ Qiao Wang @@aut@@
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author	Hanping Wan
spellingShingle	Hanping Wan misc magnetotelluric misc audio magnetotelluric misc Gulu geothermal filed misc geothermal system model misc electrical structure misc Science misc Q Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system
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topic_title	Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system magnetotelluric audio magnetotelluric Gulu geothermal filed geothermal system model electrical structure
topic	misc magnetotelluric misc audio magnetotelluric misc Gulu geothermal filed misc geothermal system model misc electrical structure misc Science misc Q
topic_unstemmed	misc magnetotelluric misc audio magnetotelluric misc Gulu geothermal filed misc geothermal system model misc electrical structure misc Science misc Q
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title	Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system
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title_full	Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system
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title_sort	electrical structure of gulu geothermal field in southern tibet and its implication for the high-temperature geothermal system
title_auth	Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system
abstract	The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs.
abstractGer	The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs.
abstract_unstemmed	The Yadong-Gulu rift (YGR) South Tibet is a Cenozoic active rift, which is endowed with abundant geothermal resources. The Gulu geothermal field (GGF) is located in the Northern section of the rift, where a large number of high-temperature hot springs develop, but its geothermal system is mysterious. In this study, the three-dimensional (3D) electrical structure of GGF is revealed by broad magnetotelluric (MT) and audio magnetotelluric (AMT). MT reveals that middle and upper crust conductors are developed in the subsurface of GGF. The conductors may originate from the partial melting that drives the geothermal system. AMT reveals that the electrical structure of GGF is conductive alternation cap overlying more resistive reservoir, which is consistent with the classical electrical structure of geothermal systems in worldwide active tectonic zones. According to the geothermal system model, cold fluids may converge from the periphery of GGF to the middle, wherein fault F1 (the Western branch of Jiulazi-Sanxung fault) may be the main channel for cold fluids to migrate downward. The fluids are heated by partial melting in the middle and upper crust, and may migrate upward along fault F2 (the middle branch of Jiulazi-Sanxung fault) and develop into heat reservoirs.
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title_short	Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system
url	https://doi.org/10.3389/feart.2023.1138360 https://doaj.org/article/5b04e8703f8a43f0b1b9f8478db9c61f https://www.frontiersin.org/articles/10.3389/feart.2023.1138360/full https://doaj.org/toc/2296-6463
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Electrical structure of Gulu geothermal field in Southern Tibet and its implication for the high-temperature geothermal system

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