, GL .Clarke and JC .Aitchison 2 D .Cluzel 3
and 1Department of Geology and Geophysics, University of Sydney, Sydney , NSW 2006,Australia 2Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong 3Laboratoire de Geologie, Universite Francaise du Pacifique, BP 4477, Noumea ,New Caledonia Corresponding author Email: geoffc@ucc.s.oz.au
ABSTRACT High-P rocks of the Pam Peninsula, NE New Caledonia, are divided into three zones: (1) an uppermost ferroglaucophane-lawsonite zone of Cretaceous to Eocene metasediments and metavolcanics of the Diahot terrane that experienced peak conditions involving P=7-9 kbar and T=400+-58oC; (2) albite-epidote-omphacite zone Diahot terrane rocks that experienced blueschist facies conditions of P=12.6+-1.2 kbar and T=570+-36oC; (3) lowermost metabasic eclogites of uncertain age that form the Pouebo terrane which experienced high-P conditions of P-23.9+-3.0 kbar and T 600oC. Eclogite occurs as metre- to kilometre-scale pods in coarse-grained hydrous mineral-rich 'glaucophanite' formed during hydration and decompression of the Pouebo terrane. Metamorphism and deformation were consequent to 44-51 Ma Eocene convergence, when sedimentary and ophiolitic nappes were thrust over the eclogites in a SW direction; white mica ages constrain metamorphism to have ended by 37+-1 Ma. Large steps in metamorphic grade are coincident with SW-dipping and NE-dipping faults that separate the three zones and were formed during two stages: (1) comparatively slow uplift and hydration of the Pouebo terrane before it was juxtaposed with the albite-epidote-omphacite zone at P 14 kbar; (2) comparatively rapid uplift of both the Pouebo terrane and the albite-epidote-omphacite zone to form a domal core of eclogite flanked by significantly lower-grade rocks to the SW and NE.
: blueschist; eclogite; high-P metamorphism; New Caledonia; thermobarometry Keywords
Pages:
843 -876
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