Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q15315> ?p ?o }
Showing triples 1 to 74 of
74
with 100 triples per page.
- Q15315 subject Q8707301.
- Q15315 subject Q8811676.
- Q15315 abstract "Schist (pronounced /ʃɪst/ SHIST) is a medium-grade metamorphic rock with medium to large, flat, sheet-like grains in a preferred orientation (nearby grains are roughly parallel). It is defined by having more than 50% platy and elongated minerals, often finely interleaved with quartz and feldspar. These lamellar (flat, planar) minerals include micas, chlorite, talc, hornblende, graphite, and others. Quartz often occurs in drawn-out grains to such an extent that a particular form called quartz schist is produced. Schist is often garnetiferous. Schist forms at a higher temperature and has larger grains than phyllite. Geological foliation (metamorphic arrangement in layers) with medium to large grained flakes in a preferred sheetlike orientation is called schistosity.The names of various schists are derived from their mineral constituents. For example, schists rich in mica are called mica schists and include biotite or muscovite. Most schists are mica schists, but graphite and chlorite schists are also common. Schists are also named for their prominent or perhaps unusual mineral constituents, as in the case of garnet schist, tourmaline schist, and glaucophane schist.The individual mineral grains in schist, drawn out into flaky scales by heat and pressure, can be seen with the naked eye. Schist is characteristically foliated, meaning that the individual mineral grains split off easily into flakes or slabs. The word schist is derived ultimately from the Greek word σχίζειν schízein meaning "to split", which is a reference to the ease with which schists can be split along the plane in which the platy minerals lie.Most schists are derived from clays and muds that have passed through a series of metamorphic processes involving the production of shales, slates and phyllites as intermediate steps. Certain schists are derived from fine-grained igneous rocks such as basalts and tuffs. Schists are frequently used as dimension stone, which is stone that has been selected and fabricated to specific shapes or sizes.".
- Q15315 thumbnail Schist_detail.jpg?width=300.
- Q15315 wikiPageExternalLink Samuels.
- Q15315 wikiPageExternalLink sgmc-unit.php?unit=IDZXmhs%3B0.
- Q15315 wikiPageWikiLink Q103223.
- Q15315 wikiPageWikiLink Q105368.
- Q15315 wikiPageWikiLink Q1057300.
- Q15315 wikiPageWikiLink Q105794.
- Q15315 wikiPageWikiLink Q106532.
- Q15315 wikiPageWikiLink Q11299.
- Q15315 wikiPageWikiLink Q1143398.
- Q15315 wikiPageWikiLink Q114675.
- Q15315 wikiPageWikiLink Q11500795.
- Q15315 wikiPageWikiLink Q119632.
- Q15315 wikiPageWikiLink Q11990990.
- Q15315 wikiPageWikiLink Q12880211.
- Q15315 wikiPageWikiLink Q134583.
- Q15315 wikiPageWikiLink Q160409.
- Q15315 wikiPageWikiLink Q16249320.
- Q15315 wikiPageWikiLink Q166409.
- Q15315 wikiPageWikiLink Q167741.
- Q15315 wikiPageWikiLink Q170258.
- Q15315 wikiPageWikiLink Q170449.
- Q15315 wikiPageWikiLink Q179911.
- Q15315 wikiPageWikiLink Q190727.
- Q15315 wikiPageWikiLink Q191360.
- Q15315 wikiPageWikiLink Q192637.
- Q15315 wikiPageWikiLink Q193450.
- Q15315 wikiPageWikiLink Q207079.
- Q15315 wikiPageWikiLink Q212895.
- Q15315 wikiPageWikiLink Q213544.
- Q15315 wikiPageWikiLink Q22693.
- Q15315 wikiPageWikiLink Q23757.
- Q15315 wikiPageWikiLink Q237883.
- Q15315 wikiPageWikiLink Q2509719.
- Q15315 wikiPageWikiLink Q316671.
- Q15315 wikiPageWikiLink Q335249.
- Q15315 wikiPageWikiLink Q413272.
- Q15315 wikiPageWikiLink Q413380.
- Q15315 wikiPageWikiLink Q42045.
- Q15315 wikiPageWikiLink Q42302.
- Q15315 wikiPageWikiLink Q423051.
- Q15315 wikiPageWikiLink Q427254.
- Q15315 wikiPageWikiLink Q429754.
- Q15315 wikiPageWikiLink Q43010.
- Q15315 wikiPageWikiLink Q43338.
- Q15315 wikiPageWikiLink Q44377.
- Q15315 wikiPageWikiLink Q47069.
- Q15315 wikiPageWikiLink Q484924.
- Q15315 wikiPageWikiLink Q525802.
- Q15315 wikiPageWikiLink Q5281656.
- Q15315 wikiPageWikiLink Q5309.
- Q15315 wikiPageWikiLink Q542715.
- Q15315 wikiPageWikiLink Q5642847.
- Q15315 wikiPageWikiLink Q582768.
- Q15315 wikiPageWikiLink Q612133.
- Q15315 wikiPageWikiLink Q660019.
- Q15315 wikiPageWikiLink Q6931872.
- Q15315 wikiPageWikiLink Q731880.
- Q15315 wikiPageWikiLink Q751300.
- Q15315 wikiPageWikiLink Q7946.
- Q15315 wikiPageWikiLink Q82658.
- Q15315 wikiPageWikiLink Q844202.
- Q15315 wikiPageWikiLink Q8707301.
- Q15315 wikiPageWikiLink Q876798.
- Q15315 wikiPageWikiLink Q8811676.
- Q15315 wikiPageWikiLink Q9129.
- Q15315 wikiPageWikiLink Q917402.
- Q15315 type Thing.
- Q15315 comment "Schist (pronounced /ʃɪst/ SHIST) is a medium-grade metamorphic rock with medium to large, flat, sheet-like grains in a preferred orientation (nearby grains are roughly parallel). It is defined by having more than 50% platy and elongated minerals, often finely interleaved with quartz and feldspar. These lamellar (flat, planar) minerals include micas, chlorite, talc, hornblende, graphite, and others.".
- Q15315 label "Schist".
- Q15315 depiction Schist_detail.jpg.