Results 171 to 180 of about 13,004 (219)
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Compressional behaviour of CaNiSi2O6 clinopyroxene: bulk modulus systematic and cation type in clinopyroxenes

Physics and Chemistry of Minerals, 2005
A single-crystal of composition CaNiSi2O6 (space group C2/c) was investigated at high pressure up to about 7.8  GPa by X-ray diffraction. The unit-cell parameters were measured at 18 different pressures. The P-V data were fitted by a third-order Birch-Murnaghan equation of state V0=435.21(1)  A3, K 0=117.6(3) GPa and K′=6.4(1).
NESTOLA F.   +3 more
openaire   +4 more sources

Machine Learning Thermo-Barometry: Application to Clinopyroxene-Bearing Magmas

open access: yesJournal of Geophysical Research: Solid Earth, 2020
We introduce a new approach, based on machine learning, to estimate pre-eruptive temperatures and storage depths using clinopyroxene-melt pairs and clinopyroxene-only chemistry.
Maurizio Petrelli   +2 more
exaly   +2 more sources

Properties of clinopyroxene LiFeGe2O6

Physics of the Solid State, 2010
The polycrystalline compound LiFeGe2O6 has been synthesized by the solid-phase reaction. The X-ray diffraction, Mossbauer, calorimetric, and magnetic investigations have been carried out. The Mossbauer spectrum at 300 K represents a single quadrupole doublet.
T. V. Drokina   +9 more
openaire   +1 more source

Raman spectroscopy of CaCoSi2O6–Co2Si2O6 clinopyroxenes

Physics and Chemistry of Minerals, 2014
Raman spectra were collected on a set of synthetic clinopyroxenes along the series CaCoSi2O6–Co2Si2O6. Changes in peak position and peak width show: (1) evidence of a phase transition from C2/c to P21/c, at Ca0.4Co1.6Si2O6, in agreement with previous X-ray observations; (2) peak broadening for intermediate compositions, with sharper peaks close to the ...
MANTOVANI, Luciana   +5 more
openaire   +3 more sources

Potassium in Clinopyroxene Inclusions from Diamonds

Science, 1991
Analytical transmission electron microscopy, electron microprobe analyses, and single-crystal x-ray diffraction data support the conclusion that high potassium contents, up to 1.5 weight percent K 2 O, of some diopside and omphacite inclusions from diamonds represent valid clinopyroxene compositions with K in solid ...
G E, Harlow, D R, Veblen
openaire   +2 more sources

Clinopyroxene dissolution in basaltic melt

Geochimica et Cosmochimica Acta, 2009
Abstract The history of magmatic systems may be inferred from reactions between mantle xenoliths and host basalt if the thermodynamics and kinetics of the reactions are quantified. To study diffusive and convective clinopyroxene dissolution in silicate melts, diffusive clinopyroxene dissolution experiments were conducted at 0.47–1.90 GPa and 1509 ...
Yang Chen, Youxue Zhang
openaire   +1 more source

Pb diffusion in clinopyroxene

Chemical Geology, 1998
Abstract Chemical diffusion of Pb under anhydrous, pO2-buffered conditions has been measured in natural clinopyroxenes of two different compositions: one a near-end-member diopside and the other of more iron-rich composition (∼40% diopside component).
openaire   +1 more source

Garnet–clinopyroxene and clinopyroxene geothermobarometry of deep mantle and crust eclogites and peridotites

Lithos, 2008
Abstract Eclogite is one of the major types of xenoliths in kimberlite. An investigation of such xenoliths provides important constraints on the distribution of P and T within the upper mantle and its chemical composition. Garnet–clinopyroxene and clinopyroxene barometers are proposed for mantle eclogites and peridotites on the basis of CaTs ...
openaire   +1 more source

Transcrystalline melt migration in clinopyroxene

Contributions to Mineralogy and Petrology, 2010
Glass inclusions in clinopyroxene phenocrysts from La Sommata (Vulcano Island, Aeolian Arc) were reheated and submitted to a sustained thermal gradient. Each remelted inclusion undergoes a transient textural and chemical reequilibration and concomitantly begins to migrate along a crystallographic direction, at a small angle with the thermal gradient ...
Sonzogni, Yann   +2 more
openaire   +2 more sources

Hydrothermal clinopyroxenes of the Skaergaard intrusion

Contributions to Mineralogy and Petrology, 1986
Magmatic augites reacted with high temperature aqueous solutions to form secondary calcic pyroxenes during the subsolidus cooling of the Skaergaard intrusion. Secondary, hydrothermal clinopyroxenes replace wall rock igneous augites at the margins of veins filled with calcic amphibole. These veins are up to several millimeters wide and tens of meters in
Manning, Craig E., Bird, Dennis K.
openaire   +1 more source

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