Results 11 to 20 of about 43,521 (279)

Origin of Isotopic Diversity among Carbonaceous Chondrites [PDF]

open access: yesThe Astrophysical Journal Letters, 2023
Carbonaceous chondrites are some of the most primitive meteorites and derive from planetesimals that formed a few million years after the beginning of the solar system.
Jan L. Hellmann   +7 more
doaj   +2 more sources

Abundance, major element composition and size of components and matrix in CV, CO and Acfer 094 chondrites [PDF]

open access: yes, 2023
The relative abundances and chemical compositions of the macroscopic components or “inclusions” (chondrules and refractory inclusions) and fine-grained mineral matrix in chondritic meteorites provide constraints on astrophysical theories of inclusion ...
D. Ebel   +9 more
semanticscholar   +1 more source

Carbon Speciation and Solubility in Silicate Melts

open access: yesGeophysical Monograph Series, Page 179-194., 2020

This book is Open Access. A digital copy can be downloaded for free from Wiley Online Library.

Explores the behavior of carbon in minerals, melts, and fluids under extreme conditions

Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon ...
Natalia Solomatova   +2 more
wiley  

+5 more sources

Thermal alteration of CM carbonaceous chondrites: Mineralogical changes and metamorphic temperatures [PDF]

open access: yes, 2021
The CM carbonaceous chondrite meteorites provide a record of low temperature aqueous reactions in the early solar system. A number of CM chondrites also experienced short-lived, post-hydration thermal metamorphism at temperatures of 200C to over 750C ...
A. King, P. Schofield, S. Russell
semanticscholar   +1 more source

The aqueous alteration of CM chondrites, a review

open access: yesGeochimica et Cosmochimica Acta, 2021
The CM chondrites are samples of primitive water-rich asteroids formed during the early solar system. They record significant interaction between liquid water and silicate rock, resulting in a mineralogy dominated by hydrated secondary phases.
M. Suttle   +4 more
semanticscholar   +1 more source

The Fe/S ratio of pyrrhotite group sulfides in chondrites: An indicator of oxidation and implications for return samples from asteroids Ryugu and Bennu

open access: yesGeochimica et Cosmochimica Acta, 2021
Determining compositional trends among individual minerals is key to understanding the thermodynamic conditions under which they formed and altered, and is also essential to maximizing the scientific value of small extraterrestrial samples, including ...
D. Schrader   +6 more
semanticscholar   +1 more source

The Osmium Isotope Signature of Phanerozoic Large Igneous Provinces

open access: yesGeophysical Monograph Series, Page 229-246., 2021

Exploring the links between Large Igneous Provinces and dramatic environmental impact

An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Alexander J. Dickson   +2 more
wiley  

+2 more sources

Hydrogen in chondrites: Influence of parent body alteration and atmospheric contamination on primordial components

open access: yesGeochimica et Cosmochimica Acta, 2020
Hydrogen occurs at the near percent level in the most hydrated chondrites (CI and CM) attesting to the presence of water in the asteroid-forming regions.
L. Vacher   +6 more
semanticscholar   +1 more source

The relationship between CM and CO chondrites: Insights from combined analyses of titanium, chromium, and oxygen isotopes in CM, CO, and ungrouped chondrites

open access: yesGeochimica et Cosmochimica Acta, 2021
A close relationship between CM and CO chondrites has been suggested by previous petrologic and isotopic studies, leading to the suggestion that they may originate from similar precursor materials or even a common parent body.
Z. Torrano   +5 more
semanticscholar   +1 more source

The most primitive CM chondrites, Asuka 12085, 12169, and 12236, of subtypes 3.0–2.8: Their characteristic features and classification

open access: yesPolar Science, 2020
CM chondrites (CMs) are the most abundant group of carbonaceous chondrites. CMs experienced varying degrees of secondary aqueous alteration and heating that modified or destroyed their primitive features. We have studied three chondrites, Asuka (A) 12085,
M. Kimura   +6 more
semanticscholar   +1 more source

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