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