Re-visiting Geothermal Fluid Circulation, Reservoir Depth and Temperature of Geothermal Springs of India
• Most of the thermal water are of immature water type. • Four major water types were identified in four major geothermal provinces. • For the Himalayan springs, water–rock interaction are dominant at depths. • The reservoir temperature of the Himalayan and the west coast springs are higher. • The f...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Goswami, Susmita [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China - Liu, Huiying ELSEVIER, 2021, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:612 ; year:2022 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.jhydrol.2022.128131 |
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| 520 | |a • Most of the thermal water are of immature water type. • Four major water types were identified in four major geothermal provinces. • For the Himalayan springs, water–rock interaction are dominant at depths. • The reservoir temperature of the Himalayan and the west coast springs are higher. • The fluid circulation depth for the Himalayas are deeper (∼2.14 km). | ||
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• Most of the thermal water are of immature water type. • Four major water types were identified in four major geothermal provinces. • For the Himalayan springs, water–rock interaction are dominant at depths. • The reservoir temperature of the Himalayan and the west coast springs are higher. • The fluid circulation depth for the Himalayas are deeper (∼2.14 km). |
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• Most of the thermal water are of immature water type. • Four major water types were identified in four major geothermal provinces. • For the Himalayan springs, water–rock interaction are dominant at depths. • The reservoir temperature of the Himalayan and the west coast springs are higher. • The fluid circulation depth for the Himalayas are deeper (∼2.14 km). |
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• Most of the thermal water are of immature water type. • Four major water types were identified in four major geothermal provinces. • For the Himalayan springs, water–rock interaction are dominant at depths. • The reservoir temperature of the Himalayan and the west coast springs are higher. • The fluid circulation depth for the Himalayas are deeper (∼2.14 km). |
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