Hydrothermal Systems Characterized by Crustal Thermally‐dominated Structures of Southeastern China
Southeastern China (SE China) is located in the Pacific tectonic domain and has experienced a series of tectonomagmatic events induced by the subduction of the Paleo‐Pacific Plate since the late Mesozoic. The subduction formed a series of NE‐NNE oriented faults under a NW–SE regional stress field, a...
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| Veröffentlicht in: | Acta geologica Sinica (Beijing) 2023-08, Vol.97 (4), p.1003-1013 |
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| container_title | Acta geologica Sinica (Beijing) |
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| creator | WANG, Guiling GAN, Haonan LIN, Wenjing YUE, Gaofan YAN, Xiaoxue LI, Tingxin ZHANG, Wei MA, Feng |
| description | Southeastern China (SE China) is located in the Pacific tectonic domain and has experienced a series of tectonomagmatic events induced by the subduction of the Paleo‐Pacific Plate since the late Mesozoic. The subduction formed a series of NE‐NNE oriented faults under a NW–SE regional stress field, along which a number of thermal springs occur. Previous studies have focused on the genesis mechanism of specific geothermal fields in SE China, but the general characteristics of hydrothermal systems in SE China remains unclear. In this study, we investigate the correlation between geothermal activity, hydrochemical type and regional faults by studying the distribution of hydrothermal activity and geochemical properties of typical hydrothermal systems in SE China. The hydrothermal systems in SE China have a crustal thermally‐dominated structural origin unique to the specific geological and tectonic conditions of the Eurasian Plate margin. The upwelling of the asthenosphere and the widespread granitoids with high radiogenic heat production in SE China provide major heat sources for regional geothermal anomalies. The NE‐oriented crustal thermally‐dominated faults are critical for the formation of geothermal anomalies and NW‐oriented extensional faults have created favorable conditions for meteoric water infiltration, transportation and the formation of thermal springs. |
| doi_str_mv | 10.1111/1755-6724.15078 |
| format | Article |
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The subduction formed a series of NE‐NNE oriented faults under a NW–SE regional stress field, along which a number of thermal springs occur. Previous studies have focused on the genesis mechanism of specific geothermal fields in SE China, but the general characteristics of hydrothermal systems in SE China remains unclear. In this study, we investigate the correlation between geothermal activity, hydrochemical type and regional faults by studying the distribution of hydrothermal activity and geochemical properties of typical hydrothermal systems in SE China. The hydrothermal systems in SE China have a crustal thermally‐dominated structural origin unique to the specific geological and tectonic conditions of the Eurasian Plate margin. The upwelling of the asthenosphere and the widespread granitoids with high radiogenic heat production in SE China provide major heat sources for regional geothermal anomalies. The NE‐oriented crustal thermally‐dominated faults are critical for the formation of geothermal anomalies and NW‐oriented extensional faults have created favorable conditions for meteoric water infiltration, transportation and the formation of thermal springs.</description><edition>English ed.</edition><identifier>ISSN: 1000-9515</identifier><identifier>EISSN: 1755-6724</identifier><identifier>DOI: 10.1111/1755-6724.15078</identifier><language>eng</language><publisher>Richmond: Wiley Subscription Services, Inc</publisher><subject>Anomalies ; Asthenosphere ; Fault lines ; Faults ; Geological faults ; geothermal activity ; Geothermal anomalies ; geothermal reservoir ; Geothermal springs ; Heat sources ; Hot springs ; Hydrothermal activity ; Hydrothermal fields ; hydrothermal system ; Hydrothermal systems ; Mesozoic ; Meteoric water ; Ocean circulation ; Plate margins ; Plates ; Plates (tectonics) ; Southeastern China ; Stress distribution ; Subduction ; Subduction (geology) ; Tectonics ; thermal lithosphere ; Upwelling ; Water infiltration ; Water springs</subject><ispartof>Acta geologica Sinica (Beijing), 2023-08, Vol.97 (4), p.1003-1013</ispartof><rights>2023 The Authors. 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The NE‐oriented crustal thermally‐dominated faults are critical for the formation of geothermal anomalies and NW‐oriented extensional faults have created favorable conditions for meteoric water infiltration, transportation and the formation of thermal springs.</description><subject>Anomalies</subject><subject>Asthenosphere</subject><subject>Fault lines</subject><subject>Faults</subject><subject>Geological faults</subject><subject>geothermal activity</subject><subject>Geothermal anomalies</subject><subject>geothermal reservoir</subject><subject>Geothermal springs</subject><subject>Heat sources</subject><subject>Hot springs</subject><subject>Hydrothermal activity</subject><subject>Hydrothermal fields</subject><subject>hydrothermal system</subject><subject>Hydrothermal systems</subject><subject>Mesozoic</subject><subject>Meteoric water</subject><subject>Ocean circulation</subject><subject>Plate margins</subject><subject>Plates</subject><subject>Plates (tectonics)</subject><subject>Southeastern China</subject><subject>Stress distribution</subject><subject>Subduction</subject><subject>Subduction (geology)</subject><subject>Tectonics</subject><subject>thermal lithosphere</subject><subject>Upwelling</subject><subject>Water infiltration</subject><subject>Water springs</subject><issn>1000-9515</issn><issn>1755-6724</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNqF0LtOwzAYBeAIgUQpzKyRGJjS2o4dJ2MVQYtUiSHdLccXmiqXYjuCdOIReEaeBJdUMOLFlvX9x9YJglsIZtCvOaSERAlFeAYJoOlZMPm9OfdnAECUEUgugytrdwAkJIFkEsjVIE3ntso0vA6LwTrV2DDfcsOFU6Y6KBmWQ5ib3joPNiOsh6-PT9k1VcudB4UzvXC9UTbsdFh0vc_jPsm0Psmb6-BC89qqm9M-DTaPD5t8Fa2fl0_5Yh1xDFEalQBlCAqKleZYAKFiwVNMaYYzCmFJpEJSlUgSnRKKYo2V1IlAmuhEQ6zjaXA_xr7xVvP2he263rT-QSYP7yVTCKAYYACgl3ej3JvutVfW_VGUkhTQBGHk1XxUwnTWGqXZ3lQNNwODgB07Z8eG2bFh9tO5n0hOP6hqNfzH2SJfFuPgNx9hhdw</recordid><startdate>202308</startdate><enddate>202308</enddate><creator>WANG, Guiling</creator><creator>GAN, Haonan</creator><creator>LIN, Wenjing</creator><creator>YUE, Gaofan</creator><creator>YAN, Xiaoxue</creator><creator>LI, Tingxin</creator><creator>ZHANG, Wei</creator><creator>MA, Feng</creator><general>Wiley Subscription Services, Inc</general><general>Technology Innovation Center for Geothermal&Hot Dry Rock Exploration and Development,Ministry of Natural Resources,Shijiazhuang,Hebei 050061,China</general><general>Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences,Shijiazhuang,Hebei 050061,China</general><scope>24P</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>202308</creationdate><title>Hydrothermal Systems Characterized by Crustal Thermally‐dominated Structures of Southeastern China</title><author>WANG, Guiling ; 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| ispartof | Acta geologica Sinica (Beijing), 2023-08, Vol.97 (4), p.1003-1013 |
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| language | eng |
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| source | Wiley Online Library Journals Frontfile Complete; Alma/SFX Local Collection |
| subjects | Anomalies Asthenosphere Fault lines Faults Geological faults geothermal activity Geothermal anomalies geothermal reservoir Geothermal springs Heat sources Hot springs Hydrothermal activity Hydrothermal fields hydrothermal system Hydrothermal systems Mesozoic Meteoric water Ocean circulation Plate margins Plates Plates (tectonics) Southeastern China Stress distribution Subduction Subduction (geology) Tectonics thermal lithosphere Upwelling Water infiltration Water springs |
| title | Hydrothermal Systems Characterized by Crustal Thermally‐dominated Structures of Southeastern China |
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