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30 years of P-T-t paths: What we’ve learned about orogenesis. Frank S. Spear Rensselaer Polytechnic Institute. (1977). Tauern Window, Austria (Selverstone et al, 1984). P-T paths from zoned garnet. Tauern Window, Austria (Selverstone et al, 1984).
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30 years of P-T-t paths:What we’ve learned about orogenesis Frank S. Spear Rensselaer Polytechnic Institute
Tauern Window, Austria (Selverstone et al, 1984) P-T paths from zoned garnet
Tauern Window, Austria (Selverstone et al, 1984)
P-T paths and nappe tectonics - New Hampshire Spear et al. (2007) Ernst, 1976
Trace element thermobarometry • Ti-in-quartz (Titaniq) • Y in garnet
Y zoning in garnet BF-17A - Western New Hampshire TM-730 - Strafford Dome, Central Vermont 4341 ppm - inner core 5346 ppm - outer core 29 ppm - rim
Y concentration in garnet + xenotime assemblages Tectonic loading at rates in excess of 8 cm/year
Diffusion studies: Rates of tectonic processes • Ti-in-quartz (Titaniq) • Mn in garnet
79-149d (New Hampshire: kyanite zone) Grt St Ky Grt
79-149d (New Hampshire: kyanite zone) CL image Grt
79-149d (New Hampshire: kyanite zone) CL image Grt
79-149D Orfordville, NH: kyanite zone CL image Qtz Grt
Peak T/Duration 550C/1.2 m.y. 575C/0.6 m.y. 600C/0.3 m.y.
TM-730 Mn zoning
TM-730 - Mn diffusion modeling 2.5 m.y. 0.25 m.y.