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Fluid Flux in Fractured Rock of the Alpine Fault Hanging‐Wall Determined from Temperature Logs in the DFDP‐2B Borehole, New Zealand

Abstract Sixteen temperature logs were acquired during breaks in drilling of the 893m‐deep DFDP‐2B borehole, which is in the Alpine Fault hanging‐wall. The logs record various states of temperature recovery after thermal disturbances induced by mud circulation. The long‐wavelength temperature signal...

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Главные авторы: Lucie Janku‐Capova, Rupert Sutherland, John Townend, Mai‐Linh Doan, Cécile Massiot, Jamie Coussens, Bernard Célérier
Формат: Artigo
Язык:Inglês
Опубликовано: Wiley 2018-08-01
Серии:Geochemistry, Geophysics, Geosystems
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Online-ссылка:https://doi.org/10.1029/2017GC007317
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