Quantitative phase petrology of cordierite-orthoamphibole gneisses and related rocks

6533b822fe1ef96bd127cbab

RESEARCH PRODUCT

Quantitative phase petrology of cordierite-orthoamphibole gneisses and related rocks

Johann F.a. Diener Richard White Roger Powell

subject

Mineral Metamorphic rock Geochemistry Geology Cordierite engineering.material Gedrite Geochemistry and Petrology Anthophyllite Whiteschist engineering Petrology Geology Terrane Gneiss

description

Cordierite-orthoamphibole gneisses and rocks of similar composition commonly contain low-variance mineral assemblages that can provide useful information about the metamorphic evolution of a terrane. New calculated petrogenetic grids and pseudosections are presented in the FeO-MgO-Al2O3-SiO2-H2O (FMASH), Na2O-CaO-K2O-FeO-MgO-Al2 O3- SiO2-H2O (NCKFMASH) and Na2O-CaO-K2O-FeO-MgO-Al2O3- SiO2-H2O-TiO2-Fe2 O3 (NCKFMASHTO) chemical systems to investigate quantitatively the phase relations in these rocks. Although the bulk compositions of cordierite-orthoamphibole gneisses are close to FMASH, calculations in this system do not adequately account for the observed range of mineral assemblages. Calculations in NCKFMASH and NCKFMASHTO highlight the role of minor constituents such as Ca, Na and Fe3+ in the mineral assemblage evolution of such rocks and these systems are more appropriate for interpreting the evolution of natural examples. © 2008 Blackwell Publishing Ltd.

year	journal	country	edition	language
2008-10-01	Journal of Metamorphic Geology

https://doi.org/10.1111/j.1525-1314.2008.00791.x

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