High‐pressure metamorphism caused by magma loading in Fiordland, New Zealand

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Abstract
Cretaceous granulite facies metamorphism in the Fiordland area of New Zealand has distinctive mineralogical, textural and structural features that set it apart from most other regional metamorphic belts. The metamorphism, developed over a 30×150‐km area and the consequence of a 20‐km‐thick increment to crustal thickness, is closely associated in space and time with a large plutonic complex, the Western Fiordland Orthogneiss (WFO). Although temperatures and pressures as high as 700 °C and 12 kbar were attained, the metamorphic overprint on earlier low‐pressure assemblages is weak and incomplete. Little strain accompanied the metamorphism. The temperature threshold at which metamorphic recrystallization is recorded is over 500 °C. Zoned garnets are preserved at unusually high temperatures, indicating duration of metamorphism on the order of 10 times shorter than in most other regional terranes. This pattern of features bears close similarity to metamorphism in the Coast Plutonic Complex in North America, where a mechanism of ‘magma loading’ has been invoked. In Fiordland, the high‐pressure metamorphism can be explained by depression of country rock under a crustal zone that is inflated by intrusion of the WFO. Regional structure of the WFO as a horizontally sheeted complex suggests that the pluton was emplaced by vertical displacement of country rock, and supports the magma loading model.

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