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Spatially-focussed melt formation in aluminous metapelites from Broken Hill, Australia

Citation

White, RW and Powell, R and Halpin, JA, Spatially-focussed melt formation in aluminous metapelites from Broken Hill, Australia, Journal of Metamorphic Geology, 22, (9) pp. 825-845. ISSN 0263-4929 (2004) [Refereed Article]


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The definitive published version is available online at: http://www3.interscience.wiley.com/

DOI: doi:10.1111/j.1525-1314.2004.00553.x

Abstract

Large garnet poikiloblasts hosted by leucosome in metapelitic gneiss from Broken Hill reflect complex mineral-melt relationships. The spatial relationship between the leucosomes and the garnet poikiloblasts implies that the growth of garnet was strongly linked to the production of melt. The apparent difficulty of garnet to nucleate a large number of grains during the prograde breakdown of coexisting biotite and sillimanite led to the spatial focussing of melting reactions around the few garnet nuclei that formed. Continued reaction of biotite and sillimanite required diffusion of elements from where minerals were reacting to sites of garnet growth. This diffusion was driven by chemical potential gradients between garnet-bearing and garnet-absent parts of the rock. As a consequence, melt and peritectic K-feldspar also preferentially formed around the garnet. The diffusion of elements led to the chemical partitioning of the rock within an overall context in which equilibrium may have been approached. Thus, the garnet-bearing leucosomes record in situ melt formation around garnet porphyroblasts rather than centimetrescale physical melt migration and segregation. The near complete preservation of the high-grade assemblages in the mesosome and leucosome is consistent with substantial melt loss. Interconnected networks between garnet-rich leucosomes provide the most likely pathway for melt migration. Decimetre-scale, coarse-grained,garnet-poor leucosomes may represent areas of melt flux through a large-scale melt transfer network. © 2004 Blackwell Publishing Ltd.

Item Details

Item Type:Refereed Article
Keywords:diffusion; granulite facies; metapelite; NCKFMASHTO; partial melting
Research Division:Earth Sciences
Research Group:Geology
Research Field:Igneous and Metamorphic Petrology
Objective Division:Expanding Knowledge
Objective Group:Expanding Knowledge
Objective Field:Expanding Knowledge in the Earth Sciences
Author:Halpin, JA (Dr Jacqueline Halpin)
ID Code:75905
Year Published:2004
Web of Science® Times Cited:117
Deposited By:Centre for Ore Deposit Research - CODES CoE
Deposited On:2012-02-20
Last Modified:2012-04-04
Downloads:1 View Download Statistics

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