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

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Presentation on theme: "30 years of P-T-t paths: What we’ve learned about orogenesis"— Presentation transcript:

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

2 (1977)

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

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

5

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

7

8 Trace element thermobarometry
Ti-in-quartz (Titaniq) Y in garnet

9 Y zoning in garnet BF-17A - Western New Hampshire
TM Strafford Dome, Central Vermont 4341 ppm - inner core 5346 ppm - outer core 29 ppm - rim

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

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

12 79-149d (New Hampshire: kyanite zone)
Grt St Ky Grt

13 79-149d (New Hampshire: kyanite zone)
CL image Grt

14 79-149d (New Hampshire: kyanite zone)
CL image Grt

15 79-149D Orfordville, NH: kyanite zone
CL image Qtz Grt

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

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

18 TM-730 Mn zoning

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

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23 10 cm/year

24 10 cm/year

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