Discussion of 'Metamorphic P - T and retrograde path of high-pressure Barrovian metamorphic zones near Cairn Leuchan, Caledonian orogen, Scotland'
dc.contributor.author | Aoki, K. | |
dc.contributor.author | Maruyama, S. | |
dc.contributor.author | Oliver, G. | |
dc.contributor.author | Omori, S. | |
dc.contributor.author | Viete, D. | |
dc.contributor.author | Wilde, Simon | |
dc.contributor.author | Windley, B. | |
dc.date.accessioned | 2018-02-01T05:22:12Z | |
dc.date.available | 2018-02-01T05:22:12Z | |
dc.date.created | 2018-02-01T04:49:10Z | |
dc.date.issued | 2014 | |
dc.identifier.citation | Aoki, K. and Maruyama, S. and Oliver, G. and Omori, S. and Viete, D. and Wilde, S. and Windley, B. 2014. Discussion of 'Metamorphic P - T and retrograde path of high-pressure Barrovian metamorphic zones near Cairn Leuchan, Caledonian orogen, Scotland'. Geological Magazine.. 151 (4): pp. 755-763. | |
dc.identifier.uri | http://hdl.handle.net/20.500.11937/62145 | |
dc.identifier.doi | 10.1017/S001675681300099X | |
dc.description.abstract |
K. Aoki, B. F. Windley, S. Maruyama & S. Omori reply: First, we thank Viete, Oliver & Wilde for their interesting and thought-provoking comments on the timing of the high-pressure granulite facies (HGR) metamorphism recorded in metamorphic rocks at Cairn Leuchan, Scotland, published by Aoki et al. (2013). Based on new metamorphic data of garnetites and garnet-amphibolites at Cairn Leuchan and new zircon U-Pb ages of amphibolitized eclogite at Tomatin, we suggested in our publication that the HGR metamorphism was retrograde after eclogite facies before the c. 470 Ma 'Barrovian metamorphism'. Viete, Oliver & Wilde however speculate that the HGR metamorphism at Cairn Leuchan may have occurred at c. 1000 Ma, as a result of their new U-Pb zircon age of the Cowhythe Gneiss at Portsoy and from previous studies of the geological structure and geochronology. We are grateful for this opportunity to describe, albeit in a preliminary manner, our new understanding and tectonic model of the Caledonian orogen in Scotland and western Ireland of which the Barrovian metamorphism is a key component. A reply to a comment is not the correct place to propose an entirely new paradigm for such a classic orogen, but we will present our model more fully in a future publication.. Copyright © Cambridge University Press 2014. | |
dc.publisher | Cambridge University Press | |
dc.title | Discussion of 'Metamorphic P - T and retrograde path of high-pressure Barrovian metamorphic zones near Cairn Leuchan, Caledonian orogen, Scotland' | |
dc.type | Journal Article | |
dcterms.source.volume | 151 | |
dcterms.source.number | 4 | |
dcterms.source.startPage | 755 | |
dcterms.source.endPage | 763 | |
dcterms.source.issn | 0016-7568 | |
dcterms.source.title | Geological Magazine. | |
curtin.department | Department of Applied Geology | |
curtin.accessStatus | Fulltext not available |
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