Intracrystalline Olivine-Ringwoodite Transformation and Time-Dependent Growth Rates.
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- Kerschhofer L.
- Bayerisches Geoinstitut, Universitaet Bayreuth
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- Liu M.
- Dept. of Earth, Atmospheric and Planetary Sciences
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- Rubie D. C.
- Bayerisches Geoinstitut, Universitaet Bayreuth
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- McConnell J. D. C.
- Dept. of Earth Sciences, University of Oxford
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- Sharp T. G.
- Dept. of Geology, Arizona State University
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- Dupas C.
- Bayerisches Geoinstitut, Universitaet Bayreuth
Bibliographic Information
- Other Title
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- Intracrystalline Olivine-Ringwoodite Tr
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Abstract
During the transformation of olivine (Fo90) to ringwoodite and wadsleyite at 18-20 GPa three transformation microstructures develop: (i) Reaction rims form around olivine by incoherent grain boundary nucleation; the growth rates of these rims decrease strongly with reaction time because the volume decrease causes elastic strain to develop. (ii) Intracrystalline, coherent ringwoodite lamellae nucleate on previously formed (100) α stacking faults. (iii) Polycrystalline ringwoodite and/or wadsleyite lenses develop in the interior of relict olivine crystals by nucleation of incoherent grains on the coherent ringwoodite lamellae. The observed intracrystalline transformation mechanism and the time-dependence of growth have important implications for predicting the depth of the olivine-spinel transformation in subducting lithosphere.
Journal
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- The Review of High Pressure Science and Technology
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The Review of High Pressure Science and Technology 7 28-33, 1998
The Japan Society of High Pressure Science and Technology
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Details 詳細情報について
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- CRID
- 1390001204381774592
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- NII Article ID
- 10002688615
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- NII Book ID
- AN10452913
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- ISSN
- 13481940
- 0917639X
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- NDL BIB ID
- 4493829
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed