Author
Listed:
- Yoshio Kono
(HPCAT, Geophysical Laboratory, Carnegie Institution of Washington, 9700 South Cass Avenue, Argonne, Illinois 60439, USA)
- Curtis Kenney-Benson
(HPCAT, Geophysical Laboratory, Carnegie Institution of Washington, 9700 South Cass Avenue, Argonne, Illinois 60439, USA)
- Daniel Hummer
(Planetary and Space Sciences, University of California Los Angeles, 595 Charles Young Drive East, Box 951567, Los Angeles, California 90095, USA)
- Hiroaki Ohfuji
(Geodynamics Research Center, Ehime University, 2–5 Bunkyo-cho, Matsuyama 790–8577, Japan)
- Changyong Park
(HPCAT, Geophysical Laboratory, Carnegie Institution of Washington, 9700 South Cass Avenue, Argonne, Illinois 60439, USA)
- Guoyin Shen
(HPCAT, Geophysical Laboratory, Carnegie Institution of Washington, 9700 South Cass Avenue, Argonne, Illinois 60439, USA)
- Yanbin Wang
(GeoSoilEnviroCARS, Center for Advanced Radiation Sources, The University of Chicago, 5640 South Ellis Avenue, Chicago, Illinois 60637, USA)
- Abby Kavner
(Planetary and Space Sciences, University of California Los Angeles, 595 Charles Young Drive East, Box 951567, Los Angeles, California 90095, USA)
- Craig E. Manning
(Planetary and Space Sciences, University of California Los Angeles, 595 Charles Young Drive East, Box 951567, Los Angeles, California 90095, USA)
Abstract
Knowledge of the occurrence and mobility of carbonate-rich melts in the Earth’s mantle is important for understanding the deep carbon cycle and related geochemical and geophysical processes. However, our understanding of the mobility of carbonate-rich melts remains poor. Here we report viscosities of carbonate melts up to 6.2 GPa using a newly developed technique of ultrafast synchrotron X-ray imaging. These carbonate melts display ultralow viscosities, much lower than previously thought, in the range of 0.006–0.010 Pa s, which are ~2 to 3 orders of magnitude lower than those of basaltic melts in the upper mantle. As a result, the mobility of carbonate melts (defined as the ratio of melt-solid density contrast to melt viscosity) is ~2 to 3 orders of magnitude higher than that of basaltic melts. Such high mobility has significant influence on several magmatic processes, such as fast melt migration and effective melt extraction beneath mid-ocean ridges.
Suggested Citation
Yoshio Kono & Curtis Kenney-Benson & Daniel Hummer & Hiroaki Ohfuji & Changyong Park & Guoyin Shen & Yanbin Wang & Abby Kavner & Craig E. Manning, 2014.
"Ultralow viscosity of carbonate melts at high pressures,"
Nature Communications, Nature, vol. 5(1), pages 1-8, December.
Handle:
RePEc:nat:natcom:v:5:y:2014:i:1:d:10.1038_ncomms6091
DOI: 10.1038/ncomms6091
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