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Elasticity of Grossular and Spessartite Garnets by Brillouin Spectroscopy
Journal of Geophysical Research: Solid Earth, 1989The single‐crystal elastic moduli of natural samples of grossular (99.0 mol % Ca3Al2Si3O12) and spessartite (94.8 mol % Mn3Al2Si3O12) have been measured by Brillouin spectroscopy under ambient conditions. From these results the adiabatic bulk moduli Ks and shear moduli μ are calculated to be Ks = 168.4 ± 0.7, μ = 108.9 ± 0.4 for grossular, and Ks = 178.
Jay D Bass
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A Phosphate-Bearing Spessartite Garnet From Wodgina, Western Australia
Gff, 1941(1941). A phosphate-bearing spessartite garnet from Wodgina, Western Australia. Geologiska Foreningen i Stockholm Forhandlingar: Vol. 63, No. 4, pp. 413-418.
Brian Mason
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Differentiation Trends of Spessartite Dikes, Sandia Mountains, New Mexico
Journal of Geology, 1970Hornblende spessartite dikes of the Sandia Mountains, New Mexico, contain small leucocratic dikelets that appear to be differentiated from the spessartite by fractional crystallization. Mineralogically the leucocratic dikelets are hornblende syenite, but chemically they more closely resemble Nockolds's (1954) average monzonite. During differentiation $$
Lee A Woodward
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Rhombohedral Magnetic Structure in Spessartite Type Garnets
Physica Status Solidi (B): Basic Research, 1973W Prandl
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Melanite from the endoskarn of a spessartite dyke intruding into the Kinshozan limestone in Ogaki City, Gifu Prefecture [PDF]
The Journal of Earth and Planetary Sciences, Nagoya University, 2011 2011A spessartite dyke that intruded into the Permian Kinshozan limestone formed endoskarn that is rich in melanite, along with clinopyroxene and apatite, in a matrix of secondary calcite, thomsonite, stilbite, heulandite and apophyllite.
SUZUKI, Kazuhiro +2 more
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Spessartite Garnet With Hexoctahedral Faces From Jail Hill, Haddam, Connecticut
Rocks and Minerals, 1960David M Seaman
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Geological Magazine, 1993
AbstractLamprophyre sills and dykes of Ordovician age were emplaced within Cambrian–Lower Ordovician sedimentary rocks around the northern margins of the Midlands Microcraton. The intrusions show internal mineralogical and chemical variations indicating emplacement as multiple intrusions of co-magmatic pulses.
R. S. Thorpe +2 more
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AbstractLamprophyre sills and dykes of Ordovician age were emplaced within Cambrian–Lower Ordovician sedimentary rocks around the northern margins of the Midlands Microcraton. The intrusions show internal mineralogical and chemical variations indicating emplacement as multiple intrusions of co-magmatic pulses.
R. S. Thorpe +2 more
openaire +2 more sources