Results 51 to 60 of about 5,656 (205)

Chondrules as direct thermochemical sensors of solar protoplanetary disk gas

open access: yesScience Advances, 2018
Cathodoluminescence reveals structures indicative of gas-assisted epitaxial growth during chondrule melt crystallization. Chondrules, millimeter-sized igneous spherules comprising the major component of most chondritic meteorites, formed during the first
G. Libourel, M. Portail
semanticscholar   +1 more source

THE Formation of chondrule-like particles in RF discharge plasma

open access: yesPhysical Sciences and Technology, 2023
Chondrules are fundamental components of chondritic meteorites and play a vital role in understanding the formation of the early solar system. This study focuses on the synthesis of chondrule-like particles in a plasma environment using a radiofrequency
Assan Abdirakhmanov   +8 more
doaj   +1 more source

The 26Al-26Mg systematics of FeO-rich chondrules from Acfer 094: two chondrule generations distinct in age and oxygen isotope ratios.

open access: yesGeochimica et Cosmochimica Acta, 2019
The 26Al-26Mg ages of FeO-rich (type II) chondrules from Acfer 094, one of the least thermally metamorphosed carbonaceous chondrites, were determined by SIMS analysis of plagioclase and olivine/pyroxene using a radio frequency (RF) plasma oxygen ion ...
A. Hertwig   +4 more
semanticscholar   +1 more source

Apatite in Bennu samples indicates multiple stages of aqueous alteration

open access: yesMeteoritics &Planetary Science, EarlyView.
Abstract Calcium phosphates are ubiquitous in planetary materials, including samples returned from asteroid Bennu by the OSIRIS‐REx mission. We characterized apatite [Ca5(PO4)3(F,Cl,OH)] grains in Bennu samples by scanning electron microscopy, electron microprobe analysis, and transmission electron microscopy to investigate their compositions, mineral ...
Laura B. Seifert   +10 more
wiley   +1 more source

Chondrule Destruction via Dust Collisions in Shock Waves

open access: yesThe Astrophysical Journal
A leading candidate for the heating source of chondrules and igneous rims is shock waves. This mechanism generates high relative velocities between chondrules and dust particles.
Yuji Matsumoto   +2 more
doaj   +1 more source

Kivesvaara C2 chondrite: silicate petrography and chemical composition [PDF]

open access: yesBulletin of the Geological Society of Finland, 1983
Fragments of the Kivesvaara meteorite were said to have been found in Paltamo, northern Finland in 1968. The chemical and mineral composition and the textural features show that this meteorite is a rare C2 carbonaceous chondrite.
K.A. Kinnunen, R. Saikkonen
doaj   +1 more source

Molybdenum isotopic evidence for the origin of chondrules and a distinct genetic heritage of carbonaceous and non-carbonaceous meteorites

open access: yes, 2016
Nucleosynthetic isotope anomalies are powerful tracers to determine the provenance of meteorites and their components, and to identify genetic links between these materials. Here we show that chondrules and matrix separated from the Allende CV3 chondrite
G. Budde   +5 more
semanticscholar   +1 more source

Can Chondrules Be Produced by the Interaction of Jupiter with the Protosolar Disk? [PDF]

open access: yesAstrophysical Journal, 2019
Chondrules are crystallized droplets of silicate melt formed by rapid heating to high temperatures (>1800 K) of solid precursors followed by hours or days of cooling.
J. Bodénan   +4 more
semanticscholar   +1 more source

Geochemical and petrographic re‐evaluation of ungrouped iron meteorites from Western Australia

open access: yesMeteoritics &Planetary Science, EarlyView.
Abstract Under the current classification scheme, ungrouped irons make up ~11% of all recognized iron meteorites. A further ~7% of iron meteorites are currently classified as simply “irons” and are yet to be fully classified. To potentially classify these meteorites, newer approaches, including either statistical modeling or advanced geochemical ...
Ashley Rogers   +6 more
wiley   +1 more source

Oxygen isotopic diversity of chondrule precursors and the nebular origin of chondrules

open access: yesEarth and Planetary Science Letters, 2018
FeO-poor (type I) porphyritic chondrules formed by incomplete melting of solid dust precursors via a yet-elusive mechanism. Two settings are generally considered for their formation: (i) a nebular setting where primordial solids were melted, e.g.
Y. Marrocchi   +4 more
semanticscholar   +1 more source

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