A. El Goresy et al., A natural shock-induced dense polymorph of rutile with alpha-PbO2 structure in the suevite from the Ries crater in Germany, EARTH PLAN, 192(4), 2001, pp. 485-495
A dense post-rutile titanium dioxide (TiO2) phase was discovered in shocked
garnet gneisses from the Ries crater by reflected-light microscopy, laser
rnicroRaman spectroscopy and micro-beam X-ray diffraction. The Raman spectr
um consists of nine bands at wave numbers: 152, 175, 285, 315, 340, 358, 42
8, 532 and 575 cm(-1). These bands are identical to those of the alpha -PbO
2-structured polymorph of TiO2 synthesized in a dynamic laboratory experime
nt. The diffraction pattern of the natural mineral revealed an orthorhombic
lattice similar to the (alpha -PbO2) polymorph with the cell parameters a
= 4,535(2) Angstrom. b = 5.499(2) Angstrom c = 4.900(2) Angstrom (space gro
up Phen; columbite-type structure), density rho =4.34g/cm(2), where the num
bers in parentheses are standard deviations in the last significant digits.
This new polymorph is 2% denser than rutile. The rutile/alpha -PbO2 polymo
rph phase transformation occurs exclusively at the grain boundaries between
rutile and the shock-compacted host biotite and advances inwards in rutile
. This textural relation establishes phase boundaries as the preferable fab
ric settings for dynamic-induced high-pressure phase transitions. Ab initio
calculations negates the formation of the alpha -PbO2 polymorph by inversi
on of a parental fluorite-structured polymorph during decompression. Heatin
g of the experimentally produced alpha -PbO2 polymorph above 500 degreesC s
hows that it inverts back in a laboratory time scale to rutile. Hence. the
survival of the alpha -PbO2-structured polymorph in naturally shocked rocks
constrains the post-shock temperature of the TiO2-bearing assemblage at an
upper bound of 500 degreesC. The presence of this dense phase is expected
in the Earth's upper mantle below 123 km. The rutile/alpha -PbO2-structured
polymorph phase transition in subducted crustal limbs in tile upper mantle
should then be accompanied by considerable changes in the partitioning and
fractionation of Nb and Ta between this TiO2 polymorph and the coexisting
dense silicates. (C) 2001 Elsevier Science B.V. All rights reserved.