Geothermal occurrence analysis of Dongying Formation in Tanggu area of Tianjin |
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Authors: | LIU Jiulong JIN Baozhen LI Yuanyuan WANG Jige YUE Liyan WANG Xi |
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Institution: | Tianjin Geothermal Exploration and Development-Designing Institute, Tianjin 300250, China |
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Abstract: | Based on introducing geological structure of Tanggu area,the authors analyzed the sedimentary envi- ronment of Paleogene Dongying Formation,and further analyzed its geothermal occurrence. The studied area spans two grade Ⅳ tectonic units which are Beitang depression and Banqiao depression. The studied area is mainly located in the Tanggu nose- like structure which is the secondary structure of Beitang depression. Its ex- istence affects the sedimentary distribution of the part strata of Paleogene. The depositions of Dongying Ⅲ (SQEd 3 ) and DongyingⅡ (SQEd 2 ) are mainly delta front facies and lake sand bars which are propitious to the geothermal fluid enrichment. The favorable enrichment region of geothermal fluid is located in south Hetou- Tanggu. Most of DongyingⅠ (SQEd 1 ) changes into swamp plain deposition, only the northeast part of this area is the distributary riverway facies with developed sand layers. There is the favorable enrichment region of geo- thermal fluid. The hydraulic connection is weak among the geothermal reservoirs of Dongying Formation and its overlying Guantao and Minghuazhen formations. The underlying Shahejie Formation geothermal reservoir pro- vides a steady stream of fluid supply and ground pressure protection for Dongying Formation geothermal reser- voir. |
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Keywords: | Dongying Formation sedimentary environment geothermal fluid enrichment condition hydraulicconnection Tanggu area |
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