Fluid inclusion evidence for recent temperature increases at Fenton Hill hot dry rock test site west of the Valles Caldera, New Mexico, U.S.A.-Reference-Cited by-同舟云学术

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Fluid inclusion evidence for recent temperature increases at Fenton Hill hot dry rock test site west of the Valles Caldera, New Mexico, U.S.A.

Published:1989-02 Issue:4 Volume:36 Page:257-266
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Sasada Masakatsu

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. Systematics of stretching of fluid inclusions I: Fluorite and sphalerite at 1 atmosphere confining pressure;Bodnar;Econ. Geol.,1984

3. Isotopic evidence for local derivation of strontium in deep-seated, fracture-filling calcite from granitic rocks in drill hole GT-2;Brookins,1976

4. Evidence from fluid inclusions for a paleogeothermal gradient at the geothermal test well site, Los Alamos, New Mexico;Burruss;J. Volcanol. Geotherm. Res.,1979

5. Paleomagnetism, potassium-argon ages, and geology of rhyolites and associated rocks of Valles Caldera, New Mexico;Doell;Geol. Soc. Am., Mem.,1968

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Fluid inclusions-Basics and recent studies-;Japanese Magazine of Mineralogical and Petrological Sciences;2003

2. Origin of a magnetic lineation on Kyushu Island, Japan;The Island Arc;1997-12

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