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- Q1813872 subject Q7037486.
- Q1813872 subject Q7163795.
- Q1813872 subject Q7163796.
- Q1813872 subject Q7468490.
- Q1813872 abstract "Stylolites or styolite (Greek: stylos, pillar; lithos, stone) are serrated surfaces within a rock mass at which mineral material has been removed by pressure dissolution, in a process that decreases the total volume of rock. Insoluble minerals, such as clays, pyrite and oxides, remain within the stylolites and make them visible. Sometime host rocks contain no insoluble minerals, in which case stylolites can be recognized by change in texture of the rock. They occur most commonly in homogeneous rocks, carbonates, cherts, sandstones, but they can be found in certain igneous rocks and ice. Their size vary from microscopic contacts between two grains (microstylolites) to large structures up to 20 m in length and up to 10 m in amplitude in ice. Stylolites usually form parallel to bedding, because of overburden pressure, but they can be oblique or even perpendicular to bedding, as a result of tectonic activity.".
- Q1813872 thumbnail Stylolites_mcr1.jpg?width=300.
- Q1813872 wikiPageExternalLink Display.cfm?Term=stylolite.
- Q1813872 wikiPageExternalLink 1038.pdf.
- Q1813872 wikiPageWikiLink Q1070438.
- Q1813872 wikiPageWikiLink Q1281067.
- Q1813872 wikiPageWikiLink Q13085.
- Q1813872 wikiPageWikiLink Q134783.
- Q1813872 wikiPageWikiLink Q163082.
- Q1813872 wikiPageWikiLink Q17148629.
- Q1813872 wikiPageWikiLink Q179177.
- Q1813872 wikiPageWikiLink Q1799034.
- Q1813872 wikiPageWikiLink Q1824696.
- Q1813872 wikiPageWikiLink Q189315.
- Q1813872 wikiPageWikiLink Q193343.
- Q1813872 wikiPageWikiLink Q2125457.
- Q1813872 wikiPageWikiLink Q2307625.
- Q1813872 wikiPageWikiLink Q23392.
- Q1813872 wikiPageWikiLink Q23757.
- Q1813872 wikiPageWikiLink Q334823.
- Q1813872 wikiPageWikiLink Q40614.
- Q1813872 wikiPageWikiLink Q42045.
- Q1813872 wikiPageWikiLink Q42250.
- Q1813872 wikiPageWikiLink Q4488518.
- Q1813872 wikiPageWikiLink Q465837.
- Q1813872 wikiPageWikiLink Q50769.
- Q1813872 wikiPageWikiLink Q622669.
- Q1813872 wikiPageWikiLink Q7037486.
- Q1813872 wikiPageWikiLink Q7163795.
- Q1813872 wikiPageWikiLink Q7163796.
- Q1813872 wikiPageWikiLink Q7468490.
- Q1813872 wikiPageWikiLink Q777913.
- Q1813872 wikiPageWikiLink Q7946.
- Q1813872 wikiPageWikiLink Q8063.
- Q1813872 wikiPageWikiLink Q806617.
- Q1813872 wikiPageWikiLink Q81659.
- Q1813872 comment "Stylolites or styolite (Greek: stylos, pillar; lithos, stone) are serrated surfaces within a rock mass at which mineral material has been removed by pressure dissolution, in a process that decreases the total volume of rock. Insoluble minerals, such as clays, pyrite and oxides, remain within the stylolites and make them visible. Sometime host rocks contain no insoluble minerals, in which case stylolites can be recognized by change in texture of the rock.".
- Q1813872 label "Stylolite".
- Q1813872 depiction Stylolites_mcr1.jpg.