G
Gary R. Huss
Researcher at University of Hawaii at Manoa
Publications - 240
Citations - 8713
Gary R. Huss is an academic researcher from University of Hawaii at Manoa. The author has contributed to research in topics: Chondrite & Chondrule. The author has an hindex of 51, co-authored 228 publications receiving 8012 citations. Previous affiliations of Gary R. Huss include University of New Mexico & University of Southern California.
Papers
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The formation and alteration of the Renazzo-like carbonaceous chondrites II: Linking O-isotope composition and oxidation state of chondrule olivine
Devin L. Schrader,Harold C. Connolly,Harold C. Connolly,Dante S. Lauretta,Kazuhide Nagashima,Gary R. Huss,Jemma Davidson,Jemma Davidson,Kenneth J. Domanik +8 more
TL;DR: In this article, the formation conditions of type-I and type-II chondrules in the Renazzo-like carbonaceous (CR) chondrites were analyzed to establish an internally consistent data set.
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Highly 15N-enriched chondritic clasts in the CB/CH-like meteorite Isheyevo
TL;DR: In this paper, the authors focus on the rare lithic clasts characterized by the presence of anhydrous silicates (chondrules, chondrule fragments, and CAIs).
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Ratio Estimation in SIMS Analysis
TL;DR: In this paper, an additive positive bias in the expectation value of the estimated ratio that is approximately equal to the true ratio divided by the counts of the denominator isotope of an individual ratio was shown.
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Heterogeneous distribution of 26Al at the birth of the solar system: Evidence from refractory grains and inclusions
A. N. Krot,Kentaro Makide,K. Nagashima,Gary R. Huss,Ryan C. Ogliore,Fred J. Ciesla,Le Yang,Eric Hellebrand,Eric Gaidos +8 more
TL;DR: In this article, it was shown that refractory objects originated in the presence of nebular gas enriched in 16O to varying degrees relative to the standard mean ocean water value: the Δ17OSMOW value ranges from approximately −16‰ to −35‰, and recorded heterogeneous distribution of 26Al in their formation region.
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Magmatic water in the martian meteorite Nakhla
TL;DR: In this article, the deuterium/hydrogen (D/H) ratio of the martian mantle has been measured using a Cameca ims 1280 ion-microprobe.