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In geology, the term glomeroporphyritic (also cumulophyritic) refers to the grouping of phenocrysts, not necessarily of the same mineral, into distinct clusters within porphyritic igneous rocks.[1]

References

  1. ^ "Archived copy". Archived from the original on 2007-02-04. Retrieved 2007-02-07.((cite web)): CS1 maint: archived copy as title (link)


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