Japan Geoscience Union Meeting 2014

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Oral

Symbol S (Solid Earth Sciences) » S-CG Complex & General

[S-CG62_2AM2] Geofluids and dynamics in subduction zones

Fri. May 2, 2014 11:00 AM - 12:45 PM 502 (5F)

Convener:*Atsushi Okamoto(Graduate School of Environmental Studies), Tatsuhiko Kawamoto(Institute for Geothermal Sciences, Graduate School of Science, Kyoto University), Ikuo Katayama(Department of Earth and Planetary Systems Science, Hiroshima University), Chair:Tatsuhiko Kawamoto(Institute for Geothermal Sciences, Graduate School of Science, Kyoto University), Atsushi Okamoto(Graduate School of Environmental Studies)

12:30 PM - 12:45 PM

[SCG62-P04_PG] Equation of state of topaz-OH in the subducted sediment under high pressure and high temperature

3-min talk in an oral session

*Mizuki NIIZATO1, Toru INOUE2, Nao CAI2, Hideki SUENAMI2, Sho KAKIZAWA2 (1.Department of Earth Sciences, Ehime University, 2.Geodynamics Research Center, Ehime Univercity)

Keywords:topaz-OH, high pressure hydrous phase, subducting slab, equation of state, synchrotron X-ray in-situ experiment

Dehydration reactions of hydrous minerals in the subducted sediment produce a H2O-rich fluid which causes generations of magma, decreases of melting temperature of sediment, and variations of magma compositions. Topaz-OH [Al2SiO4(OH)2], which is one of hydrous minerals, is considered to be existed in the sediment of the subducting slab. Topaz-OH is the end-member of natural topaz [Al2SiO4(OH,F)2]. The stability field of topaz-OH extends to 1500 degree C at 5-10 GPa (Wunder et al., 1993; Ono. 1998; Schmidt et al., 1998). The equation of state (EoS) for the natural topaz has been also estimated (Komatsu et al., 2003; Gatta et al., 2003). However, the EoS of the end-member topaz-OH has not been performed yet. In this study, we performed in situ X-ray diffraction (XRD) experiments under high pressure and high temperature for determining the thermal elastic properties of topaz-OH.The starting material of topaz-OH was synthesized at 10 GPa and ~1000 degree C from the quench experiment using multi-anvil apparatus. The high pressure (3-8 GPa) and high temperature (up to 800 degree C) in situ XRD experiments were carried out using MAX80 installed at beam-line NE5C at PF-AR, KEK, Japan. These XRD patterns were collected by the energy dispersive method. Thermal elastic properties were calculated from EoS fit v5.2 software (Angel, 2000) using 3rd order Birch-Murnaghan EoS.From in situ XRD experiments, we successfully determined thermal elastic properties using all-data for fixed K'=4 as below: V0=354.7(1)Å3, K0=169.8(22)GPa, (dKT/dT)P=-0.013(7) GPaK-1, a0=1.61(23)×10-5K-1, b0=1.36(41)×10-8K-2. From the detailed analysis of compression data, we found the change of the compression properties near 7 GPa. This change was also seen in a- and b-axis. Therefore we re-calculated the thermal elastic properties using two data sets: (I) below 7 GPa (II) above 7 GPa at room temperature. These calculation results from low pressure data show V0=355.2(1)Å3, K0=160.1(2)GPa, however those from the high pressure data show V0=356.5(9)Å3, K0=153.1(89) GPa (K'=4 fixed). Compared to the natural topaz, topaz-OH shows relatively large volume and bulk modulus. This shows that the volume and bulk modulus increase with increasing OH content. Compared bulk modulus with density, topaz-OH locates near the line for Birch's law and indicates large bulk modulus and density as same as Phase D [Mg2SiO4(OH)2]. We suggest that high density topaz-OH enhances the slab subduction and transports water to deeper earth's interior.