2009 Fiscal Year Final Research Report
Fluid flow and mineral precipitation within fractures under crustalenvironments
Project/Area Number |
20740304
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Research Category |
Grant-in-Aid for Young Scientists (B)
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Allocation Type | Single-year Grants |
Research Field |
Petrology/Mineralogy/Science of ore deposit
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Research Institution | Tohoku University |
Principal Investigator |
OKAMOTO Atsushi Tohoku University, 大学院・環境科学研究科, 助教 (40422092)
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Project Period (FY) |
2008 – 2009
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Keywords | 水熱反応実験 / 石英 |
Research Abstract |
Fractures play as dominant fluid pathways in the Earth's crust. Mineral veins, that are fractures sealed by minerals (i.e. quartz and calcite) show a variety of microtextures. In this study, we conducted hydrothermal experiments to precipitation of silica minerals under crustal conditions. We clarified that mechanisms and textural developments in precipitation of silica minerals systematically vary depending on Si concentration, minor elements in solutions and rock substrates.
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[Journal Article] Determination of amphibole fracture strength for quantitative paleostress analysis using microboudinage structures.2010
Author(s)
Kimura, N., Nakayama S., Tsukishima, K., Miwa, S., Okamoto, A., Masuda, T.
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Journal Title
Journal of Structural Geology 32
Pages: 136-150
Peer Reviewed
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[Presentation] Precipitation of silica minerals by hydrothermal flow-through experiments at 200-430 °C and 30 MPa.2008
Author(s)
Okamoto, A., Shaishu, H., Hirano, N., Watanabe, N., Tsuchiya, N.
Organizer
Geothermal Resource Council
Place of Presentation
Reno, Nevada
Year and Date
2008-10-07
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