Abstract
Most asteroidal igneous rocks are eucrite-like basalts and gabbros, composed mostly of ferroan low- and high-Ca pyroxenes and calcic plagioclase, plus smaller amounts of silica (most commonly tridymite), ilmenite, chromite, troilite, Ca-phosphate, metal and sometimes ferroan olivine. Eucrite-like mafic rocks are fragments of the crusts of differentiated asteroids, and most are likely from 4 Vesta.
| Original language | English |
|---|---|
| Title of host publication | 49th Lunar and Planetary Science Conference 2018 |
| Publication status | Published - 19 Mar 2018 |
Fingerprint
Dive into the research topics of 'Fine-Scale Variations in Eucritic Pyroxene FeO/MnO: Process vs. Provenance.'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver