Serpentinization of the Acoje massif, Zambales ophiolite, Philippines: hydrogen and oxygen isotope geochemistry-Reference-Cited by-同舟云学术

Serpentinization of the Acoje massif, Zambales ophiolite, Philippines: hydrogen and oxygen isotope geochemistry

Published:1989-10 Issue:1-3 Volume:168 Page:101-107
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Sturchio N.C,Abrajano T.A,Murowchick J.B,Muehlenbachs K

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference27 articles.

1. The petrology and low-temperature geochemistry of the sulfide-bearing mafic-ultramafic units of the Acoje Massif, Zambales Ophiolite, Philippines: characterization of mineral and fluid equilibria;Abrajano,1984

2. Zambales Ophiolite I. Geology and petrology of the critical zone of the Acoje Massif;Abrajano;Tectonophysics,1989

3. The relationship between fluids in some fresh alpine-type ultramafics and possible modern serpentinization;Barnes;Geol. Soc. Am. Bull.,1969

4. Serpentinization of oceanic peridotites: temperature dependence of mineralogy and boron content;Bonatti;Earth Planet. Sci. Lett.,1984

5. The use of bromine pentafluoride in the extraction of oxygen from oxides and silicates for isotopic analysis;Clayton;Geochim. Cosmochim. Acta,1963

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