HR: 17:05h
AN: T24A-05 INVITED     [Abstracts]
TI: Microstructures Developed During Natural and Experimental Decompression of Peridotite From Pressures of 10-15 GPa
AU: * Green, H W
EM: harry.green@ucr.edu
AF: Dept. of Earth Sciences, Univ. of California, Riverside, CA 92521 United States
AU: * Green, H W
EM: harry.green@ucr.edu
AF: Inst. of Geophys. and Planet. Phys., Univ. of California, Riverside, CA 92521 United States
AU: Dobrzhinetskaya, L F
EM: larissa@ucr.edu
AF: Dept. of Earth Sciences, Univ. of California, Riverside, CA 92521 United States
AB: Evidence is now robust that continental rocks and sediments can be subducted to P $>$ 6 GPa during continental collision and returned to the surface. Moreover, mantle rocks exhumed with this subducted material carry evidence of P $>$ 9 GPa and perhaps much more. We present a short review of natural examples and discuss them in the context of decompression experiments conducted on garnet lherzolite over the range 14 $\rightarrow$ 5 GPa. Experiments at 14 GPa dissolved all enstatite (En) and about 85% diopside (Di) into garnet, yielding run products of 40% Ol + 55% Grt + 5% Di. Re-annealing this product at 13 or 12 GPa resulted in exsolution of Di as blebs at garnet grain boundaries and oriented platelets of Ol chemistry within grt. Specimens first equilibrated at 8 GPa dissolved abundant En but little Di. When re-annealed at 5 GPa, En exsolved as blebs at garnet boundaries -- very similar to interstitial blebs of enstatite along grt grain boundaries in UHP ($>$200 km) Norwegian grt-harzburgite. In the latter rocks, abundant En and rare Di exsolution lamellae are also found in the cores of large garnets. Our experiments do not show such lamellae, supporting the arguments of van Roermund and Drury (1998) that they are produced only in the cores of large grains and that the interstitial pyroxenes found in their specimens are also exsolution products. Ol has not been reported with exsolution morphology in natural UHP products, nor did we observe it in our experiments at P = 5 GPa. On the other hand, our observation that Ol may be exsolved during decompression of majoritic garnet during decompression at higher P is consistent with expansion of the garnet field at the expense of wadsleyite at P $>$ 13 GPa reported by Ringwood (1991). Di, En, and/or Ol do occur along grain boundaries within larger polycrystalline garnets and within embayments at the margins of smaller amoeboid garnets in subduction zone garnet peridotites. Such garnets also may contain rounded, non-oriented, inclusions of each of these minerals, or all three together, consistent with the results of majoritic garnet decompression presented above. Our results suggest that some Ol in this microstructure may have exsolved during decompression of majoritic garnet.
DE: 8102 Continental contractional orogenic belts
DE: 8124 Earth's interior--composition and state (old 8105)
DE: 5112 Microstructure
DE: 3630 Experimental mineralogy and petrology
DE: 3924 High-pressure behavior
SC: Tectonophysics [T]
MN: 2004 AGU Fall Meeting