Ultralow velocities of amorphous CaCO3 and the origin of seismic anomalies in the Earth's upper mantle
ID:76 View Protection:ATTENDEE Updated Time:2021-06-07 16:31:31 Hits:2276 Oral Presentation

Start Time:2021-07-10 16:40(Asia/Shanghai)

Duration:15min

Session:S8 8、地球物理 » S8-18、地球物理-1

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Abstract
Volatiles (H2O, CO2, etc.) modulate the global climate in geological time. Hydrous minerals and fluids have been predominantly believed to be the major cause of the seismic low velocity, electrical conductivity abnormalities, deep earthquake, partial melting, and magma chamber for volcanoes in the upper mantle. By contrast, the effect of CO2 carriers has largely been underestimated. Calcium carbonate (CaCO3) is a major long-term host for CO2 and the nature of CaCO3 at extreme pressure-temperature (P-T) conditions are indispensable to decipher its circulation between the Earth's interior and its surface via volcanoes and subduction. Using the pulse-echo-overlap method in a Paris-Edinburgh press coupled with X-ray diffraction, we explored the seismic velocities of CaCO3 and observed an anomalously drop associated with aragonite to amorphous phase transition under P-T conditions relevant to subducting slabs in the upper mantle. Compared to aragonite, the velocity reductions of the partially amorphous CaCO3 are approximately 35% and 52% for compressional (VP) and shear (VS) wave velocities, respectively, at 3.5–5.5 GPa and 1,073–1,373 K. The VP and VS values of the partially amorphous CaCO3 are about 1/2 and 1/3 of those of the upper mantle minerals, respectively. Amorphous CaCO3-bearing domains would be expected to dwell atop the subducting slabs and naturally account for many enigmatic characteristics of the low-velocity layers in circum-Pacific subduction zones.
Keywords
deep carbon recycle,amorphization,high pressure,low velocity zone,sound velocity
Speaker
侯明强
中国科学院精密测量研究院

Submission Author
侯明强 中国科学院精密测量研究院
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    Jul 09

    2021

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    Jul 11

    2021

  • May 30 2021

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  • May 30 2021

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  • May 30 2021

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  • Jul 10 2021

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  • Jul 11 2021

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Sponsored By
青年地学论坛理事会
Organized By
中国科学院地球化学研究所
贵州大学
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