Results 1 to 10 of about 1,213,951 (200)

Latitude-dependent oxygen fugacity in arc magmas [PDF]

open access: yesNature Communications
The redox state of arc mantle has been considered to be more oxidized and diverse than that of the mid-ocean ridge, but the cause of the variation is debated.
Fangyang Hu   +5 more
doaj   +4 more sources

Sulfur degassing at Erta Ale (Ethiopia) and Masaya (Nicaragua) volcanoes: Implications for degassing processes and oxygen fugacities of basaltic systems [PDF]

open access: yesGeochemistry, Geophysics, Geosystems, 2013
We investigate the relationship between sulfur and oxygen fugacity at Erta Ale and Masaya volcanoes. Oxygen fugacity was assessed utilizing Fe3+/∑Fe and major element compositions measured in olivine‐hosted melt inclusions and matrix glasses.
J. M. deMoor   +13 more
doaj   +3 more sources

Europium in plagioclase-hosted melt inclusions reveals mantle melting modulates oxygen fugacity [PDF]

open access: yesNature Communications
To gain insights into the composition and heterogeneity of Earth’s interior, the partial pressure of oxygen (oxygen fugacity, or fO2) in igneous rocks is characterized. A surprising observation is that relative to reference buffers, fO2s of mantle melts (
Nicholas Dygert   +2 more
doaj   +2 more sources

A more reduced mantle beneath the lunar South Pole–Aitken basin [PDF]

open access: yesNature Communications
The oxygen fugacity (fO2) of the lunar mantle is of pivotal significance in comprehending the formation and evolution of the Moon. However, the fO2 of the lunar farside mantle remains unknown due to the lack of samples returned from the farside. Here, we
Huijuan Zhang   +16 more
doaj   +2 more sources

Trivalent titanium in high-titanium lunar ilmenite [PDF]

open access: yesNature Communications
Lunar mare basalts are often rich in titanium, hosted predominantly within the mineral ilmenite (Fe2+Ti4+O3). Here, we examine ilmenite in a  ~ 3.8 billion-year-old mare basalt (Apollo rock 75035) using high-resolution electron microscopy and electron ...
Advik D. Vira   +15 more
doaj   +2 more sources

Determination of oxygen fugacity from ore-bearing magma responsible for Gazu copper mineralization: Cerium data in zircon mineral [PDF]

open access: yesپترولوژی, 2021
Porphyry Cu deposits are typically oxidized. Oxygen fugacity (fO2) is a key factor, which controls the formation of porphyry Cu deposits. Trace element compositions of Cretaceous magmatic zircon grains (65.9-65.1 Ma) were determined from ore-bearing ...
Alireza Almasi   +2 more
doaj   +1 more source

Petrology and Tectonic Geophysics of Massive and Foliated Eclogites in the North Qilian Orogenic Belt: Changes in Mineral Composition, Oxygen Fugacity, and Fabric during Exhumation

open access: yesAdsorption Science & Technology, 2022
The North Qilian orogenic belt is a typical area of “cold” subduction of the early Paleozoic oceanic plate, forming a series of high pressure and low temperature metamorphic rock assemblages. Among them, eclogite is a kind of protolith, which is basaltic
Feng Wang, Daorong Zhou, Xunhua Zhang
doaj   +1 more source

Oxidation-induced nanolite crystallization triggered the 2021 eruption of Fukutoku-Oka-no-Ba, Japan

open access: yesScientific Reports, 2023
Nanometer-sized crystals (nanolites) play an important role in controlling eruptions by affecting the viscosity of magmas and inducing bubble nucleation.
Kenta Yoshida   +10 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

A new method to quantitatively control oxygen fugacity in externally heated pressure vessel experiments [PDF]

open access: yesEuropean Journal of Mineralogy, 2020
Oxygen fugacity (fO2) is a fundamental variable affecting phase equilibrium in magmas, and in externally heated pressure vessel experiments it is typically controlled by using redox buffer assemblages.
A. Alex, Z. Zajacz
doaj   +1 more source

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