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• 12:17 5 oct 2025 CatharineEudy7 discusión contribs. creó la página 1911 Encyclopædia Britannica Variolites (Página creada con «<br>Other variolites are glassy or partly crystalline facies of olivine-free dolerites, occurring as thin dikes or intrusions, or at the margins of [https://www.purevolume.com/?s=dolerite%20masses dolerite masses]. In these the felspars are well crystallized as thin rods, with square or forked ends, radiating outwards from a centre. They are commonly oligoclase, and sometimes assume branching or [https://santo.kr:443/bbs/board.php?bo_table=free&wr_id=306178 Derila Sl…»)