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- W2348406915 abstract "The average geothermal flow in the Bohai Sea waters is (60.9±8.7)mW/m2.It is up to 70~80 mW/m2 in the Shijiutuo,Shaleitian and Bonan uplifts,65-75 mW/m2 in the Bozhong sag,the Huanghekou sag and the Qinnan uplift,while lower than 65 mW/m2 in the Liaodong bay,Miaoxi,the Laizhou bay,Qikou,Sha'nan and Chengbei.The geothermal gradient varies in different structural units of the Bohai Sea waters and averages at 30.8℃/km.Higher geothermal gradient 32-42℃/km,is tested in the Shaleitian uplift,Bozhong,the Laizhou bay,Qikou,Sha'nan and Chengbei.In contrast,it is low in the sags,22-32℃/km on average.The distribution of geothermal field coincides with the structural configuration in the Bohai Sea waters,roughly reflecting the structural form of the NNE-trending Tan-Lu Fault." @default.
- W2348406915 created "2016-06-24" @default.
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- W2348406915 date "2009-01-01" @default.
- W2348406915 modified "2023-09-23" @default.
- W2348406915 title "Distribution features of current geothermal field in the Bohai Sea waters" @default.
- W2348406915 hasPublicationYear "2009" @default.
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