2016
DOI: 10.1016/j.gr.2016.08.005
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Protracted (~ 30 Ma) eclogite-facies metamorphism in northern Victoria Land (Antarctica): Implications for the geodynamics of the Ross/Delamerian Orogen

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Cited by 31 publications
(45 citation statements)
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“…The latter unit contains tectonic lenses of eclogite, amphibolite and meta‐ultramafic rock (Di Vincenzo et al., ; Ricci et al., ). The eclogite outcrops only occur along a ridge near the Husky Pass, which has served as an obvious target for many previous studies (Figure a; Capponi, Castelli, Fioretti, & Oggiano, ; Di Vincenzo et al., ; Ghiribelli, Frezzotti, & Palmeri, ; Palmeri, Frezzotti, Godard, & Davies, ; Palmeri, Talarico, & Ricci, ). In addition, one garnet‐bearing ultramafic rock was reported near the Mt.…”
Section: Geological Backgroundmentioning
confidence: 99%
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“…The latter unit contains tectonic lenses of eclogite, amphibolite and meta‐ultramafic rock (Di Vincenzo et al., ; Ricci et al., ). The eclogite outcrops only occur along a ridge near the Husky Pass, which has served as an obvious target for many previous studies (Figure a; Capponi, Castelli, Fioretti, & Oggiano, ; Di Vincenzo et al., ; Ghiribelli, Frezzotti, & Palmeri, ; Palmeri, Frezzotti, Godard, & Davies, ; Palmeri, Talarico, & Ricci, ). In addition, one garnet‐bearing ultramafic rock was reported near the Mt.…”
Section: Geological Backgroundmentioning
confidence: 99%
“…The eclogite and its retrograde product, eclogitic amphibolite, are collectively named here as the Lanterman Range eclogite, and occur in the field as: elongate layers or tabular sheets alternating with (garnet–)phengite‐bearing quartzofeldspathic schists and gneisses (Figure b); and deformed lenses or boudins, up to tens of metres thick, enveloped by the felsic gneisses (Figure c; Capponi et al., ; Ricci et al., ). Previous workers reported two distinctive types and clockwise P–T–t paths of the Lanterman Range eclogite: (a) ‘hot’ eclogites metamorphosed at ~750–850°C but undergone the amphibolite facies retrogression (Di Vincenzo & Palmeri, ; Di Vincenzo et al., ) and (b) ‘tepid’ eclogites recording quartz‐stable peak conditions at ~17–24 kbar and 700°C, preceded by prograde epidote–amphibolite facies metamorphism at ~9 kbar and 600°C (Di Vincenzo et al., ). The high ‐P metamorphism of ‘hot’ eclogites was dated at c .…”
Section: Geological Backgroundmentioning
confidence: 99%
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