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- Q488715 subject Q7153706.
- Q488715 subject Q7468490.
- Q488715 abstract "A xenomorph (also: allotriomorph) is a mineral that did not develop its otherwise typical external crystal form because of late crystallization between earlier formed crystals. Xenomorphs are typical of matrix minerals in rapidly crystallizing volcanic lavas and shallow igneous intrusions. It is also typical of the interstitial or cementing minerals formed during the diagenesis of sedimentary rocks. The opposite is an idiomorph in which the external form is controlled only by the internal crystal structure.".
- Q488715 thumbnail Quarz_xenomorph.JPG?width=300.
- Q488715 wikiPageWikiLink Q1463013.
- Q488715 wikiPageWikiLink Q180621.
- Q488715 wikiPageWikiLink Q40157.
- Q488715 wikiPageWikiLink Q42045.
- Q488715 wikiPageWikiLink Q43533.
- Q488715 wikiPageWikiLink Q488640.
- Q488715 wikiPageWikiLink Q7153706.
- Q488715 wikiPageWikiLink Q7468490.
- Q488715 wikiPageWikiLink Q7946.
- Q488715 wikiPageWikiLink Q8072.
- Q488715 wikiPageWikiLink Q82480.
- Q488715 wikiPageWikiLink Q895901.
- Q488715 type Thing.
- Q488715 comment "A xenomorph (also: allotriomorph) is a mineral that did not develop its otherwise typical external crystal form because of late crystallization between earlier formed crystals. Xenomorphs are typical of matrix minerals in rapidly crystallizing volcanic lavas and shallow igneous intrusions. It is also typical of the interstitial or cementing minerals formed during the diagenesis of sedimentary rocks.".
- Q488715 label "Xenomorph (geology)".
- Q488715 differentFrom Q488640.
- Q488715 depiction Quarz_xenomorph.JPG.