Добірка наукової літератури з теми "Polymineralic rocks"
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Статті в журналах з теми "Polymineralic rocks"
Handy, Mark R. "The solid-state flow of polymineralic rocks." Journal of Geophysical Research 95, B6 (1990): 8647. http://dx.doi.org/10.1029/jb095ib06p08647.
Повний текст джерелаJordan, Peter. "The rheology of polymineralic rocks — an approach." Geologische Rundschau 77, no. 1 (February 1988): 285–94. http://dx.doi.org/10.1007/bf01848690.
Повний текст джерелаTakeda, Yoshi-Taka. "Flow in rocks modelled as multiphase continua: application to polymineralic rocks." Journal of Structural Geology 20, no. 11 (November 1998): 1569–78. http://dx.doi.org/10.1016/s0191-8141(98)00043-1.
Повний текст джерелаLinckens, Jolien, Marco Herwegh, and Othmar Müntener. "Linking temperature estimates and microstructures in deformed polymineralic mantle rocks." Geochemistry, Geophysics, Geosystems 12, no. 8 (August 2011): n/a. http://dx.doi.org/10.1029/2011gc003536.
Повний текст джерелаSchofield, P. F., S. J. Covey-Crump, I. C. Stretton, M. R. Daymond, K. S. Knight, and R. F. Holloway. "Using neutron diffraction measurements to characterize the mechanical properties of polymineralic rocks." Mineralogical Magazine 67, no. 5 (October 2003): 967–87. http://dx.doi.org/10.1180/0026461036750138.
Повний текст джерелаHunter, Nicholas J. R., R. F. Weinberg, C. J. L. Wilson, V. Luzin, and S. Misra. "Quartz deformation across interlayered monomineralic and polymineralic rocks: A comparative analysis." Journal of Structural Geology 119 (February 2019): 118–34. http://dx.doi.org/10.1016/j.jsg.2018.12.005.
Повний текст джерелаHenry, Bernard. "Modelling the relationship between magnetic fabric and strain in polymineralic rocks." Physics of the Earth and Planetary Interiors 70, no. 3-4 (March 1992): 214–18. http://dx.doi.org/10.1016/0031-9201(92)90185-x.
Повний текст джерелаLarre, Chloé, Yann Morizet, Catherine Guillot-Deudon, Fabien Baron, and Nicolas Mangold. "Quantitative Raman calibration of sulfate-bearing polymineralic mixtures: a S quantification in sedimentary rocks on Mars." Mineralogical Magazine 83, no. 1 (September 14, 2018): 57–69. http://dx.doi.org/10.1180/mgm.2018.147.
Повний текст джерелаMikhailova, Julia A., Yakov A. Pakhomovsky, Ekaterina A. Selivanova, and Alena A. Kompanchenko. "Polymineralic Inclusions in Loparite-(Ce) from the Lovozero Alkaline Massif (Kola Peninsula, Russia): Hydrothermal Association in Miniature." Minerals 13, no. 6 (May 23, 2023): 715. http://dx.doi.org/10.3390/min13060715.
Повний текст джерелаUzel, Jessica, Yves Lagabrielle, Serge Fourcade, Christian Chopin, Pierre Monchoux, Camille Clerc, and Marc Poujol. "The sapphirine-bearing rocks in contact with the Lherz peridotite body: New mineralogical data, age and interpretation." BSGF - Earth Sciences Bulletin 191 (2020): 5. http://dx.doi.org/10.1051/bsgf/2019015.
Повний текст джерелаДисертації з теми "Polymineralic rocks"
Semeniuk, Trudi Ann. "A new descriptive methodology and study of polymineralic fault rocks from reactivated shear zones of the Ivrea Zone, Northern Italy /." [Zürich], 2003. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=15247.
Повний текст джерелаMandolini, Tommaso. "Microstructural evolution of polymineralic aggregates deformed under high pressure and temperature : an in-situ and post-mortem study on olivine+serpentine." Electronic Thesis or Diss., Université de Lille (2022-....), 2022. http://www.theses.fr/2022ULILR047.
Повний текст джерелаAt plate tectonic boundaries, the lithosphere is deformed and strain localization occurs up to kilometers-scale, which can manifest in form of shear zones. The strain localization suggests the strength of the lithosphere is locally weakened. The formation of interconnected layers of weaker minerals in the lithosphere is a potential mechanism to achieve such weakening. Serpentinized peridotite is commonly found within and between tectonic plates. It is mainly composed of olivine and serpentine minerals. The latter is generally accepted to be weaker than olivine at geological strain rates. During deformation, strain is thus expected to preferentially partition into serpentine than into olivine. This can lead to the formation of interconnected weak layers (IWL) of serpentine where strain localizes.The present work is based on microstructural investigation to infer the strain accommodation in rocks. Olivine+serpentine aggregates with two compositions (10 and 20 vol.% serpentine) are used as a proxy for partially serpentinized peridotites. The aggregates are experimentally deformed in torsion at high pressures (HP, > 2 GPa) and high temperatures (HT, > 300°C) at an equivalent strain rate of 10-4 s-1. The experiments are coupled with in-situ absorption contrast X-ray tomography. I obtain 2D and 3D information on connectivity and structural layering in the microstructure of the ‘weak' serpentine. Electron microscopy is performed on recovered samples to link the in-situ X-ray tomography observations to the plastic properties of the phases.I first outline experimental and image-data processing procedures specific to in-situ HP experimental deformation. Then, I study the deformation of the aggregates with increasing shear deformation at multiple scales of observations. The main aim is to observe the onset and development of IWL in its microstructure. The relations between the morphology and plastic properties of the phases in the rock are investigated to understand the strain localization in serpentinized peridotite.The main results show the deformation regime in olivine+serpentine aggregates can be described as semi-brittle, with the dominant phase of olivine (‘stronger') mainly displaying brittle deformation, whereas the serpentine (‘weaker') showing a dominant ductile-style deformation. A strain γ of ca. 4-5, serpentine content of ca. 20 vol.%, and initial fraction of large clusters >15 vol.% determine the condition for IWL configuration in the olivine+serpentine aggregates. Conversely, at serpentine content of ca. 10 vol.%, IWL do not occur, independently of strain or initial clusters size distribution of serpentine. This is more consistent with a load-bearing framework (LBF) behavior, where the stronger olivine grains are jammed, and during deformation crush one another, leading to grain size reduction and accommodating much of the deformation in the rock. These findings suggest contents of serpentine >10 vol.% or ca. 20 vol.% define a threshold for crucial changes in the morphology, connectivity, percolation, of the weak serpentine in serpentinized peridotites under shear. This may lead to important changes in deformation behavior and mechanical properties of the rock.In light of these findings, I give some perspectives for strain localization and shear zones initiation in the lithosphere
Частини книг з теми "Polymineralic rocks"
Shapakidze, Elena, Marina Avaliani, Marine Nadirashvili, Vera Maisuradze, Ioseb Gejadze, Tamar Petriashvili, and Evgeni Khuchua. "Assessment of the Durability of Geopolymer Materials Based on Thermally Modified Polymineral Clay Rocks." In Environmental Technology and Sustainability, 127–37. New York: Apple Academic Press, 2024. http://dx.doi.org/10.1201/9781003397960-7.
Повний текст джерелаТези доповідей конференцій з теми "Polymineralic rocks"
Economou, John, Gabriele Casale, and Jamie S. F. Levine. "EXTRACTION OF EBSD QUARTZ DEFORMATION FABRIC DOMAINS IN POLYMINERALIC ROCKS USING THE MTEX TOOLBOX FOR MATLAB." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339426.
Повний текст джерелаFeldman, V. I. "High-Pressure Polymorphic Modifications of Minerals in the Products of Impact Metamorphism of Polyminerals Rocks." In ZABABAKHIN SCIENTIFIC TALKS - 2005: International Conference on High Energy Density Physics. AIP, 2006. http://dx.doi.org/10.1063/1.2337240.
Повний текст джерелаBeljatinskaja, I. V., V. V. Milyavskiy, L. V. Sazonova, T. I. Borodina, D. M. Zhernokletov, A. Z. Zhuk, Mark Elert, et al. "SHOCK METAMORPHISM OF HORNBLENDE AND PLAGIOCLASE IN CONDITIONS OF STEP-LIKE COMPRESSION OF POLYMINERAL ROCKS." In SHOCK COMPRESSION OF CONDENSED MATTER - 2007: Proceedings of the Conference of the American Physical Society Topical Group on Shock Compression of Condensed Matter. AIP, 2008. http://dx.doi.org/10.1063/1.2832976.
Повний текст джерелаАйзенштадт, А. М., Ю. В. Соколова, Т. А. Дроздюк, and М. А. Авдушева. "INTERPHASE OF BUILDING COMPOSITIONS." In «АКТУАЛЬНЫЕ ВОПРОСЫ СОВРЕМЕННОЙ НАУКИ: ТЕОРИЯ, ТЕХНОЛОГИЯ, МЕТОДОЛОГИЯ И ПРАКТИКА». Международная научно-практическая онлайн-конференция, приуроченная к 60-ти летию член-корреспондента Академии наук ЧР, доктора технических наук, профессора Сайд-Альви Юсуповича Муртазаева. Crossref, 2021. http://dx.doi.org/10.34708/gstou.conf..2021.78.24.008.
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