A conceptual model of the Tianjin geothermal system based on isotopic studies |
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Authors: | Wang Kun Zhu Jialing |
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Affiliation: | 1.Tianjin Geothermal Exploration & Development Institute, 300250, Tianjin, China ;2.Tianjin Geothermal Research & Training Centre, Tianjin University, 300070, Tianjin, China ; |
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Abstract: | The isotopic technique is an effective measure to set up the conceptual model of a hydrothermal system. A deep circular geothermal system exists in Tianjin, including the semi-open and semi-closed karst geothermal subsystem in the bedrock and closed porous water subsystem in the clastic rocks. The geothermal water is originated from the ancient precipitation of 21-10 kaBP. Since Holocene epoch, the geothermal water is sealed for heating up. The mainly feeding channels are the karst conduits in weathered carbonate rocks of Proterozoic and Lower Paleozoic. |
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