Results 11 to 20 of about 12,575 (215)

Clinopyroxene Dissolution Records Rapid Magma Ascent [PDF]

open access: yesFrontiers in Earth Science, 2020
Magma ascent rates control volcanic eruption styles. However, the rates at which basaltic magmas ascend through the crust remain highly uncertain. Although recent studies have successfully exploited records of decompression driven degassing to estimate ...
David A. Neave, John Maclennan
doaj   +12 more sources

An olivine-clinopyroxene geothermometer

open access: yesContributions to Mineralogy and Petrology, 1976
The olivine-clinopyroxene (Fe-Mg partition) geothermometer of Powell and Powell (1974) was derived on the basis of clinopyroxene mixing parameters which imply a large miscibility gap in CaFeSi2O6-CaMgSi2O6-CaAl2SiO6 clinopyroxenes at 950° C. Application of the Powell and Powell thermometer in an empirical way (ignoring likely errors in mixing ...
Powell, Roger, Powell, Marjorie
openaire   +2 more sources

Trace element thermometry of garnet-clinopyroxene pairs [PDF]

open access: yes, 2016
We present major and trace element data on coexisting garnet and clinopyroxene from experiments carried out between 1.3 and 10 GPa and 970 and 1400 °C.
JD Blundy (15955763)   +2 more
core   +9 more sources

ThiloBissbort/Hydrogen-clinopyroxene-equilibration: Hydrogen Clinopyroxene Equilibration

open access: yes, 2022
This supplementary material contains all MATLAB© programs that have been written to model non-isothermal diffusion of hydrogen in clinopyroxene along geotherms (P-T-fO2 path)
ThiloBissbort
core   +1 more source

Natural Clinopyroxene Reference Materials for in situ Sr Isotopic Analysis via LA-MC-ICP-MS

open access: yesFrontiers in Chemistry, 2020
Clinopyroxene is a major host mineral for lithophile elements in the mantle lithosphere, and therefore, its origin is vital for constraints on mantle evolution and melt generation. In situ Sr isotopic measurement of clinopyroxene has been available since
Han Zhao   +28 more
doaj   +1 more source

Crystallization conditions of two adjacent epidote + diopside-bearing granitic stocks, northeastern Brazil

open access: yesAnais da Academia Brasileira de Ciências, 2021
The Tamboril and Olho d’Água granitic stocks are part of the abundant calc-alkalic magmatic epidote-bearing granitic rocks in the Cachoeirinha–Salgueiro Terrane (CST) in the Transversal Zone Domain, northeastern Brazil. The equigranular Olho d’Água stock
RENAN SIQUEIRA   +2 more
doaj   +1 more source

Retrogression of ultrahigh-pressure eclogite, Western Gneiss Region, Norway [PDF]

open access: yesEuropean Journal of Mineralogy, 2023
The Western Gneiss Region (WGR) in western Norway exposes ultrahigh-pressure (UHP) eclogites that occur repeatedly, within an area of high-pressure (HP) eclogites, without evidence of being separated by tectonic shear or ductile flow structures.
D. Spengler   +4 more
doaj   +1 more source

Estimation of physicochemical properties and tectonic environment of gabbro masses from‏ ‏south of Germi city (Ardabil province)‎ based on the chemistry of clinopyroxene crystals [PDF]

open access: yesپترولوژی, 2018
The studied gabbroic rocks, trending northwest- southeast, outcropped in the south of Germi, northwest of Iran. These rocks composed of plagioclase, clinopyroxene and iddingsitic olivines.
gholamreza ahmadzadeh   +1 more
doaj   +1 more source

Mafic alkaline metasomatism in the lithosphere underneath East Serbia: evidence from the study of xenoliths and the host alkali basalts [PDF]

open access: yes, 2010
Effects of mafic alkaline metasomatism have been investigated by a combined study of the East Serbian mantle xenoliths and their host alkaline rocks.
H. Downes   +9 more
core   +1 more source

Zoned Pyroxenes as Prospectivity Indicators for Magmatic Ni-Cu Sulfide Mineralization

open access: yesFrontiers in Earth Science, 2020
Small intrusions dominated by olivine- and pyroxene-rich cumulates are well known to be favorable hosts to magmatic Ni-Cu-(Platinum Group Element—PGE) sulfide mineralization.
Louise Schoneveld   +8 more
doaj   +1 more source

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