Anti-clockwise P-T paths in the lower crust: an example from a kyanite-bearing regional aureole, George Sound, New Zealand

作者：Clarke G L^*; Fitzherbert J A; Milan L A; Daczko N R; Degeling H S

来源：Journal of Metamorphic Geology, 2010, 28(1): 77-96.

DOI：10.1111/j.1525-1314.2009.00854.x

• Fiordland
• George Sound
• high-P amphibolite facies
• P-T path
• regional aureole
• Western Fiordland Orthogneiss

The George Sound Paragneiss (GSP) represents a rare Permo-Triassic unit in Fiordland that occurs as a km-scale pillar to gabbroic and dioritic gneiss of c. 120 Ma Western Fiordland Orthogneiss (WFO). It is distinguished from Palaeozoic paragneiss common in western Fiordland (Deep Cove Gneiss) by SHRIMP and laser-ablation U-Pb ages as young as c. 190 Ma and 176Hf/177Lu > 0.2828 for detrital zircon grains. The Mesozoic age of the GSP circumvents common ambiguity in the interpretation of Cretaceous v. Palaeozoic metamorphic assemblages in the Deep Cove Gneiss. A shallowly dipping S(1) foliation is preserved in the GSP distal to the WFO, cut by 100 m scale migmatite contact zones. All units preserve a steeply dipping S(2) foliation. S(1) staurolite and sillimanite inclusions in the cores of metapelitic garnet grains distal to the WFO preserve evidence for prograde conditions of T < 650 degrees C and P < 8 kbar. Contact aureole and S(2) assemblages include Mg-rich, Ca-poor cores to garnet grains in metapelitic schist that reflect WFO emplacement at approximate to 760 degrees C and approximate to 6.5 kbar. S(2) kyanite-bearing matrix assemblages and Ca-enriched garnet rims reflect approximate to 650 degrees C and approximate to 11 kbar. Poorly oriented muscovite-biotite intergrowths and rare paragonite reflect post-S(2) high-P retrogression and cooling. Pseudosection modelling in NCKFMASH defines a high-P anti-clockwise P-T history for the GSP involving: (i) mid-P amphibolite facies conditions; preceding (ii) thermal metamorphism adjacent to the WFO; followed by (iii) burial to high-P and (iv) high-P cooling induced by tectonic juxtaposition of cooler country rock.

• 出版日期2010-1