Fluid geochemistry and soil gas fluxes (CO2–CH4–H2S) at a promissory Hot Dry Rock Geothermal System: The Acoculco caldera, Mexico

Author:

Peiffer L.,Bernard-Romero R.,Mazot A.,Taran Y.A.,Guevara M.ORCID,Santoyo E.

Funder

DGAPA-UNAM

CEMIE-GEO Conacyt-SENER

Fondo Mixto Conacyt-Gobierno del Estado de Hidalgo

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference78 articles.

1. Elevated carbon dioxide flux at the Dixie Valley geothermal field, Nevada; relations between surface phenomena and the geothermal reservoir;Bergfeld;Chem. Geol.,2001

2. Carbon dioxide and hydrogen sulfide degassing and cryptic thermal input to Brimstone Basin, Yellowstone National Park, Wyoming;Bergfeld;Chem. Geol.,2012

3. Nuevos datos geoquímicos de yacimientos geotermales de alta temperatura del cinturón volcánico mexicano: Isótopos de helio, boro, nitrógeno y elementos traza;Bernard-Romero,2008

4. Assessment of the enhanced geothermal system resource base of the United States;Blackwell;Nat. Resour. Res.,2006

5. Soil gas flux exploration at the Rotokawa geothermal field and White Island, New Zealand;Bloomberg,2012

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