Evidence from fluid inclusions for a paleogeothermal gradient at the geothermal test well sites, Los Alamos, New Mexico

Author:

Burruss R.C.,Hollister L.S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference31 articles.

1. Temperature measurements in the Precambrian section of geothermal test hole No. 2;Albright;Los Alamos Scientific Laboratory Rep., La-6022-MS,1975

2. The ternary systems constituted by mercuric chloride, water, and an alkaline-earth chloride or cupric chloride;Bassett;J. Chem. Soc. (London),1933

3. Transformation of hydrates into unstable hydrates;Berthorsson,1972

4. Rb-Sr, K-Ar and fission track geochronological studies of samples from LASL drill holes, GT-1, GT-2, and EE-1;Brookins;Los Alamos Scientific Laboratory Rep., LA-6829-MS,1977

5. Comparison of past and present geothermal waters, from a study of fluid inclusions, Broadlands Field, New Zealand;Browne;EOS, Trans. Am. Geophys. Union,1974

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