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Contrasting P–T–t paths for Neoproterozoic metamorphism in MacRobertson and Kemp Lands, east Antarctica

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Halpin, JA and Clarke, GL and White, RW and Kelsey, DE (2007) Contrasting P–T–t paths for Neoproterozoic metamorphism in MacRobertson and Kemp Lands, east Antarctica. Journal of Metamorphic Geology, 25 (6). pp. 683-701.

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Abstract

Mineral equilibria modelling and electron microprobe chemical dating of monazite in granulite facies metapelitic assemblages from the MacRobertson Land coastline, Rayner Complex, east Antarctica, are consistent with an "anticlockwise" Neoproterozoic P–T–t path. Metamorphism occurred at c. 990–970 Ma, achieving peak conditions of 850 ºC and 5.6–6.2 kbar at Cape Bruce, and 900 ºC and 5.4–6.2 kbar at the Forbes Glacier ~50 km to the east. These peak metamorphic conditions preceded the emplacement of regionally extensive syntectonic charnockite. High temperature conditions are likely to have been sustained for 80 Myr by lithospheric thinning and repeated pluton emplacement; advection was accompanied by crustal thickening to maximum pressures of 6–7 kbar, followed by near-isobaric cooling. This P–T–t path is distinct from that of rocks in adjacent Kemp Land, ~50 km to the west, where a "clockwise" P–T–t path from higher-P conditions at c. 940 Ma may reflect the response of a cratonic margin displaced from the main magma flux. In this scenario, crustal shortening was initially accommodated in younger, fertile crust (MacRobertson Land) involving metasediments and felsic plutons with the transfer of strain to adjacent older crust (Kemp Land) subsequent to charnockite emplacement.

Item Type: Article
Keywords: electron microprobe monazite dating; granulite; NCKFMASHTO; pseudosection; Rayner Complex
Journal or Publication Title: Journal of Metamorphic Geology
Page Range: pp. 683-701
Identification Number - DOI: 10.1111/j.1525-1314.2007.00723.x
Additional Information:

The definitive version is available at www.blackwell-synergy.com

Date Deposited: 26 May 2008 02:34
Last Modified: 18 Nov 2014 03:41
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