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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Detalhes bibliográficos

Principais autores:	Lucie Janku‐Capova, Rupert Sutherland, John Townend, Mai‐Linh Doan, Cécile Massiot, Jamie Coussens, Bernard Célérier
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2018-08-01
coleção:	Geochemistry, Geophysics, Geosystems
Assuntos:	permeability groundwater hydrogeology geothermal aquifer
Acesso em linha:	https://doi.org/10.1029/2017GC007317
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