By B. Goscombe 1 , R.S. Blewett , K. Czarnota , P.B. Groenewald and R. Maas .
ISBN-10: 1921498935
ISBN-13: 9781921498930
ISBN-10: 1921498943
ISBN-13: 9781921498947
ISBN-10: 1921498951
ISBN-13: 9781921498954
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Extra resources for Metamorphic Evolution and Integrated Terrane Analysis of the Eastern Yilgarn Craton: Rationale, Methods, Outcomes and Interpretation
Example text
Limit of all garnet). 3 (Pattison, 2003). Maximum-T/minimum-P limit of general garnet. Reaction 3: Minimum-T limit of wet melting in metabasite (Wyllie and Wolf, 1993). Reaction 4: Minimum-T limit of clinopyroxene, for HM-buffer (Spear, 1981b). Reaction 5: Experimental minimum-T limit of orthopyroxene, for WM- and QFM-buffers (Spear, 1981b; Nair and Chacko, 2000). Reaction 6: Experimental minimum-P limit of titanite, for WM-buffer (Spear, 1981b). e QFM and HM at lower P). Reaction 7: Experimental minimum-P limit of garnet, for quartz-tholeiite B with XMg=60% (Green and Ringwood, 1967a).
Secondly, correlations between kinematics at different times with different stretching lineation directions need to be made. The dataset of Blewett and Czarnota (2005) constitutes the only broad-scale age-correlated kinematic data, and could form the basis for calibrating the kinematic array for different deformation events. GRANITOIDS HFSE Granitoids High field-strength element granites and minor granodiorites form a minor (5-10%) component of the juvenile EYC crust and are almost absent from the remainder of the Yilgarn Craton (Champion and Cassidy, 2007).
METAMORPHIC GRADIENTS AS A TECTONIC TOOL Classification of Metamorphic Gradients Metamorphic gradients are first order variables that are dependent upon the tectonic setting and crustal architecture of orogens. Consequently, metamorphic gradients offer a unique way to encompass a whole orogenic system and have the potential to act as discriminatory tools to determine palaeo-tectonic setting in metamorphic belts. Metamorphic gradients are simply the variation in metamorphic variables (pressure – P, temperature – T and temperature/depth ratio – G) of approximately the same age from a common metamorphic cycle, with respect to a length scale.
Metamorphic Evolution and Integrated Terrane Analysis of the Eastern Yilgarn Craton: Rationale, Methods, Outcomes and Interpretation by B. Goscombe 1 , R.S. Blewett , K. Czarnota , P.B. Groenewald and R. Maas .
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