Abstract
Minerals trapped as inclusions within other host minerals can develop residual stresses on exhumation as a result of the differences between the thermo-elastic properties of the host and inclusion phases. The determination of possible entrapment pressures and temperatures from this residual stress requires the mutual elastic relaxation of the host and inclusion to be determined. Previous estimates of this relaxation have relied on the assumption of linear elasticity theory. We present a new formulation of the problem that avoids this assumption. We show that for soft inclusions such as quartz in relatively stiff host materials such as garnet, the previous analysis yields entrapment pressures in error by the order of 0.1 GPa. The error is larger for hosts that have smaller shear moduli than garnet.
© 2014 by Walter de Gruyter Berlin/Boston
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Artikel in diesem Heft
- Highlights and Breakthroughs. Pauling’s rules, in a world of non-spherical atoms
- Highlights and Breakthroughs. Theoretical and applied implications of the structural order of irradiated vermiculite
- Highlights and Breakthroughs. An examination of the Ti-in-quartz thermobarometer in rocks that contain dynamically recrystallized quartz: Re-equilibration of [Ti] during recrystallization
- The Second Conference on the Lunar Highlands Crust and New Directions. Visible-infrared spectral properties of iron-bearing aluminate spinel under lunar-like redox conditions
- The Second Conference on the Lunar Highlands Crust and New Directions. VNIR spectral variability of the igneous stratified Stillwater Complex: A tool to map lunar highlands
- The Second Conference on the Lunar Highlands Crust and New Directions. Spinel-rich lithologies in the lunar highland crust: Linking lunar samples with crystallization experiments and remote sensing
- The Second Conference on the Lunar Highlands Crust and New Directions. Phosphate-halogen metasomatism of lunar granulite 79215: Impact-induced fractionation of volatiles and incompatible elements
- The Second Conference on the Lunar Highlands Crust and New Directions. Reflectance spectroscopy of plagioclase-dominated mineral mixtures: Implications for characterizing lunar anorthosites remotely
- The Second Conference on the Lunar Highlands Crust and New Directions. The distribution of Mg-spinel across the Moon and constraints on crustal origin
- The occurrence and composition of chevkinite-(Ce) and perrierite-(Ce) in tholeiitic intrusive rocks and lunar mare basalt
- Garnet as a major carrier of the Y and REE in the granitic rocks: An example from the layered anorogenic granite in the Brno Batholith, Czech Republic
- Mid-infrared optical constants of clinopyroxene and orthoclase derived from oriented single-crystal reflectance spectra
- Time-resolved synchrotron X-ray diffraction study of the dehydration behavior of chalcophanite
- Ab initio investigations of dioctahedral interlayer-deficient mica: Modeling particles of illite found within gas shale
- Trona at extreme conditions: A pollutant-sequestering material at high pressures and low temperatures
- In-situ U-Th/Pb geochronology of (urano)thorite
- Temperature-induced amorphization of Na-zeolite A: A view from multi-nuclear high-resolution solid-state NMR
- “Silicified” pyrochlore from nepheline syenite (mariupolite) of the Mariupol Massif, SE Ukraine: A new insight into the role of silicon in the pyrochlore structure
- Physio-chemical properties of gamma-irradiated vermiculite and their significance for radiation protection and thermoluminescence
- Ti resetting in quartz during dynamic recrystallization: Mechanisms and significance
- Thermodynamic study of monoclinic pyrrhotite in equilibrium with pyrite in the Ag-Fe-S system by solid-state electrochemical cell technique
- Phase diagram and P-V-T equation of state of Al-bearing seifertite at lowermost mantle conditions
- Crystal structure of Guinier-Preston zones in orthopyroxene: Z-contrast imaging and ab inito study
- Crystal chemistry and surface configurations of two polylithionite-1M crystals
- Crystal chemistry of synthetic Ti-Mg-bearing hibonites: A single-crystal X-ray study
- Mineralogy and crystal chemistry of Mn, Fe, Co, Ni, and Cu in a deep-sea Pacific polymetallic nodule
- Agakhanovite-(Y), ideally (YCa)⃞2KBe3Si12O30, a new milarite-group mineral from the Heftetjern pegmatite, Tørdal, Southern Norway: Description and crystal structure
- Actinides in Geology, Energy, and the Environment. Ichnusaite, Th(MoO4)2·3H2O, the first natural thorium molybdate: Occurrence, description, and crystal structure
- Actinides in Geology, Energy, and the Environment. Quantification of α-particle radiation damage in zircon
- What Lurks in the Martian Rocks and Soil? Investigations of Sulfates, Phosphates, and Perchlorates. Spectral properties of Ca-sulfates: Gypsum, bassanite, and anhydrite
- What Lurks in the Martian Rocks and Soil? Investigations of Sulfates, Phosphates, and Perchlorates. Flower-like apatite recording microbial processes through deep geological time and its implication to the search for mineral records of life on Mars
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- Letter. Identification of hydrogen defects linked to boron substitution in synthetic forsterite and natural olivine
- Letter. Densified glasses as structural proxies for high-pressure melts: Configurational compressibility of silicate melts retained in quenched and decompressed glasses
- Letter. Geobarometry from host-inclusion systems: The role of elastic relaxation
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