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30 years of P-T-t paths: What we’ve learned about orogenesis

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

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  1. 30 years of P-T-t paths:What we’ve learned about orogenesis Frank S. Spear Rensselaer Polytechnic Institute

  2. (1977)

  3. Tauern Window, Austria (Selverstone et al, 1984) P-T paths from zoned garnet

  4. Tauern Window, Austria (Selverstone et al, 1984)

  5. P-T paths and nappe tectonics - New Hampshire Spear et al. (2007) Ernst, 1976

  6. Trace element thermobarometry • Ti-in-quartz (Titaniq) • Y in garnet

  7. 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

  8. Y concentration in garnet + xenotime assemblages Tectonic loading at rates in excess of 8 cm/year

  9. Diffusion studies: Rates of tectonic processes • Ti-in-quartz (Titaniq) • Mn in garnet

  10. 79-149d (New Hampshire: kyanite zone) Grt St Ky Grt

  11. 79-149d (New Hampshire: kyanite zone) CL image Grt

  12. 79-149d (New Hampshire: kyanite zone) CL image Grt

  13. 79-149D Orfordville, NH: kyanite zone CL image Qtz Grt

  14. Peak T/Duration 550C/1.2 m.y. 575C/0.6 m.y. 600C/0.3 m.y.

  15. TM-730 - Central VT. Staurolite-Kyanite zone

  16. TM-730 Mn zoning

  17. TM-730 - Mn diffusion modeling 2.5 m.y. 0.25 m.y.

  18. 10 cm/year

  19. 10 cm/year

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