- For example, olivine may form the primary phenocrysts of some materials, and as such is used to define the subtype of that material (e.g.
- Analcime phenocrysts in igneous rocks: Primary or secondary
- American Mineralogist, Volume 78, pages 225-229, 1993. Analcime phenocrysts in igneous rocks: Primary or secondary?-Discussion.
- Melt Inclusions in Olivine Phenocrysts: Using Diffusive Re
- that large unzoned cores of high-Fo phenocrysts cannot reflect diffusive phenocrysts.
- Silver Spruce Reports More Significant REE Results Pope's Hill Trend, Trans
- The mineralized unit, a syenite to monzonite, a minimum of 10 metres wide, carries green pyroxene crystals as phenocrysts up to 5 cm long, and is open along strike to both the east and west.
- Phenocryst - Wikipedia, the free encyclopedia
- A phenocryst is a relatively large and usually conspicuous crystal distinctly larger than the grains of the rock groundmass of a porphyritic igneous rock.
- Large crystals, or phenocrysts, of feldspar in a basalt flow.
- Phenocrysts - definition of Phenocrysts by the Free Online Dictionary
- A conspicuous, usually large, crystal embedded in porphyritic igneous rock. [ pheno- + cryst(al).] phe no·crys tic adj.
Phenocrysts is described in multiple online sources, as addition to our editors' articles, see section below for printable documents, Phenocrysts books and related discussion.
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