Cultural advice

The Australian National University acknowledges, celebrates and pays our respects to the Ngunnawal and Ngambri people of the Canberra region and to all First Nations Australians on whose traditional lands we meet and work, and whose cultures are among the oldest continuing cultures in human history.

Aboriginal and Torres Strait Islander peoples are advised that ANU Library collections may include images, names, voices, and other representations of deceased persons.

Material in the collection may contain terms, language or views that reflect the period in which the item was created and may be considered inappropriate today.

Internal and external fluid sources for eclogite-facies veins in the Monviso Meta-ophiolite, Western Alps: Implications for fluid flow in subduction zones

Date

Authors

Spandler, Carl

Pettke, Thomas

Rubatto, Daniela

Publisher

Oxford University Press

Abstract

To contribute to our understanding of the mechanisms and pathways of fluid movement through deeply subducted crust, we investigate high-pressure veins cutting eclogite-facies (~2·0 GPa and ~600°C) metagabbros of the Monviso Ophiolite, Italian Western Al

Keywords

Keywords: chemical composition; chromium; eclogite; facies; fluid flow; garnet; geochemistry; host rock; isotopic composition; metagabbro; metamorphism; ophiolite; petrology; serpentinite; subduction zone; zircon; Alps; Western Alps Eclogite; Fluid; Monviso; Serpentinite; Subduction; Veins

URI

http://hdl.handle.net/1885/70680

Collections

ANU Research Publications

Source

Journal of Petrology

Type

Journal article

DOI

10.1093/petrology/egr025

Restricted until

2037-12-31

Downloads

File

Description

01_Spandler_Internal_and_external_fluid_2011.pdf (2.22 MB)