Chondrules and other components in C, O, and E chondrites: Similarities in their properties and origins

ERD Scott, GJ Taylor - Journal of Geophysical Research: Solid …, 1983 - Wiley Online Library
We describe three types of chondrules that are common to H3, LL3, CM2, CO3, and CV3
chondrites. Low and high‐FeO, porphyritic olivine chondrules contain olivine with Fa0. 3–8 …
被引用次数：203 相关文章

Chondrules and other components in C, O, and E chondrites Similarities in their properties and origins

ERD Scott, GJ Taylor - Journal of Geophysical Research, Supplement, 1983 - ntrs.nasa.gov
Three types of chondrules are described that are common to H3, LL3, CM2, CO3, and CV3
chondrites. Low-and high-FeO, porphyritic olivine chondrules contain olivine with Fa0. 3-8 …
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[HTML][HTML] Chondrules and other components in C, O, and E chondrites Similarities in their properties and origins

ERD Scott, GJ Taylor - … Union and NASA, Lunar and Planetary …, 1983 - adsabs.harvard.edu
Three types of chondrules are described that are common to H3, LL3, CM2, CO3, and CV3
chondrites. Low-and high-FeO, porphyritic olivine chondrules contain olivine with Fa0. 3-8 …

Chondrules and other components in C, O, and E chondrites: Similarities in their properties and origins

ERD Scott, GJ Taylor - Journal of Geophysical Research: Solid Earth, 1983 - cir.nii.ac.jp
抄録< jats: p> We describe three types of chondrules that are common to H3, LL3, CM2,
CO3, and CV3 chondrites. Low and high‐FeO, porphyritic olivine chondrules contain olivine …