2014 GSA Annual Meeting in Vancouver, British Columbia (19–22 October 2014)

Paper No. 89-11
Presentation Time: 10:45 AM

THE TEMPO OF CONTINENTAL MARGIN ARC CONSTRUCTION AND EXTENSIONAL OROGENIC COLLAPSE: A DEEP-CRUSTAL PERSPECTIVE FROM FIORDLAND, NEW ZEALAND


SCHWARTZ, Joshua J.1, STOWELL, Harold H.2, KLEPEIS, Keith A.3, TULLOCH, Andy4, COBLE, Matthew A.5, KYLANDER-CLARK, Andrew6 and HACKER, Brad6, (1)Department of Geological Sciences, California State University Northridge, 18111 Nordhoff Street, Northridge, CA 91330, (2)Department of Geological Sciences, University of Alabama, Tuscaloosa, AL 35487, (3)Geology, University of Vermont, Trinity Campus, Burlington, VT 05405, (4)GNS Science, Dunedin, 1930, New Zealand, (5)Department of Geological Sciences, Stanford University, Stanford, CA 94305, (6)Geological Sciences, UC, Santa Barbara, Department of Geological Sciences, UC Santa Barbara—Building 526, Santa Barbara, CA 93106-9630

The exhumed root of the Fiordland orogen offers a deep-crustal view into the life cycle of a continental-margin arc from magmatic construction to extensional orogenic collapse. We integrate U-Pb and Sm-Nd geo- and thermochronologic data from zircon, garnet, titanite, and rutile with structural observations from >1200 km2of the arc root to document the tempo of deep-crustal magmatism, high-temperature metamorphism, extension and cooling in central Fiordland.

Results from U-Pb SHRIMP-RG zircon geochronology reveal two principal phases of Cretaceous, deep-crustal plutonism at ca. 125-120 Ma and 118-115 Ma. The latter phase of magmatism resulted in the emplacement of nearly 70% of the arc root and constituted a major flux of high Sr/Y magmas. Metamorphic zircon from Paleozoic host orthogneisses, trondhjemitic leucosomes and garnet reaction zones yield ages of 119-117 Ma, and metamorphic zircons from calc-silicates yield ages of 116-112 Ma. Garnet TIMS Sm-Nd ages from Cretaceous orthogneisses, garnet-reaction zones and trondhjemitic leucosomes range from 115-110 Ma. Outcrop- and microstructural-scale observations indicate that granulite-facies shearing initiated at ca. 116-110 Ma resulting in widely distributed zones of lower crustal flow. These data signify that regional granulite-facies metamorphism was partially synchronous with deep-crustal magmatism, partial melting and high-temperature, crystal-plastic deformation.

Titanite LASS chronology of calc-silicates and mafic orthogneisses yielded uniform ages of 113-110 Ma, suggesting rapid cooling of the arc root from ca. 900 to ~650°C in <10 Ma. Metamorphic zircon rims from Doubtful Sound indicate a pulse of amphibolite-facies metamorphism at 106 Ma that may coincide with the development of organized networks of upper amphibolite-facies shear zones. In the Resolution Island region, metamorphic zircons yield ages of 93-89 Ma implying a separate, localized pulse of amphibolite-facies metamorphism in the southwestern sector of central Fiordland. Rutile ages from both regions as old as 89 Ma signifying slow cooling (~5°C/Ma) and residence of the arc root above amphibolite-facies conditions for >20 Ma (110-89 Ma). These conditions and slow cooling facilitated extensional orogenic collapse leading to the opening of the Tasman Sea at 83 Ma.