The use of porphyroblasts to resolve the history of macro-scale structures: an example from the Robertson River Metamorphics, North-Eastern Australia
Cihan, M., and Parsons, A. (2005) The use of porphyroblasts to resolve the history of macro-scale structures: an example from the Robertson River Metamorphics, North-Eastern Australia. Journal of Structural Geology, 27 (6). pp. 1027-1045.
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The successions of inclusion trail asymmetries defining foliation intersection/inflection axes (FIAs) preserved in porphyroblasts document the geometry of deformation associated with folding and fabric development during discrete episodes of bulk shortening and suggest that deformation histories are commonly more complex than previously considered. A succession of four FIAs trending ENE–WSW, E–W, N–S and NE–SW has been distinguished based upon relative timing plus inclusion texture and orientation in the Proterozoic Robertson River Metamorphics (Georgetown Inlier, Qld, Australia). The successions of asymmetries formed around these FIAs bear no relationship to the geometry of macroscale folds present in the area suggesting that these folds predate porphyroblast growth, the widespread metamorphism and matrix fabric development. The onset of regional macro-scale folding may have begun soon after the deposition at around 1655 Ma in the Georgetown Inlier as opposed to the previously suggested date of 1570 Ma. These folds were then amplified, overturned and refolded during NNW–SSE, N–S, E–W and NW–SE directed regional bulk shortening. Earlier deformations were erased from the matrix because of bedding-induced shearing (reactivation) on the limbs of pre-existing macro-scale folds. Four foliations, S1–S4, identified in the matrix provided information about the youngest deformations preserved in these rocks. These results also suggest that existing tectonothermal models regarding the NE Australian Craton should be reconsidered.
|Item Type:||Article (Refereed Research - C1)|
|Keywords:||Georgetown inlier; Robertson River Metamorphics; foliation intersection/inflection axes (FIA); porphyroblasts; inclusion trails; deformation partitioning|
|FoR Codes:||04 EARTH SCIENCES > 0403 Geology > 040312 Structural Geology @ 100%|
|SEO Codes:||97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 100%|
|Deposited On:||29 Nov 2010 15:30|
|Last Modified:||15 Jun 2013 01:23|
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|Citation Counts with External Providers:||Web of Science: 15|
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