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- Q5455231 subject Q7037486.
- Q5455231 abstract "Fissility or Fissionability (American English) refers to the property of rocks to split along planes of weakness into thin sheets. This is commonly observed in shales, which are sedimentary rocks, and in slates and phyllites, which are foliated metamorphic rocks. The fissility in these rocks is caused by the preferred alignment of platy phyllosilicate grains due to compaction, deformation or new mineral growth. A highly fissile rock splits easily along the cleavage.".
- Q5455231 thumbnail Muzeum_Złota_w_Złotoryi_fyllit_Panenska_Hůrka_21.07.2011_p.jpg?width=300.
- Q5455231 wikiPageWikiLink Q1414356.
- Q5455231 wikiPageWikiLink Q178977.
- Q5455231 wikiPageWikiLink Q1990218.
- Q5455231 wikiPageWikiLink Q207079.
- Q5455231 wikiPageWikiLink Q457931.
- Q5455231 wikiPageWikiLink Q47069.
- Q5455231 wikiPageWikiLink Q525802.
- Q5455231 wikiPageWikiLink Q7037486.
- Q5455231 wikiPageWikiLink Q731880.
- Q5455231 wikiPageWikiLink Q751300.
- Q5455231 wikiPageWikiLink Q8063.
- Q5455231 wikiPageWikiLink Q82480.
- Q5455231 comment "Fissility or Fissionability (American English) refers to the property of rocks to split along planes of weakness into thin sheets. This is commonly observed in shales, which are sedimentary rocks, and in slates and phyllites, which are foliated metamorphic rocks. The fissility in these rocks is caused by the preferred alignment of platy phyllosilicate grains due to compaction, deformation or new mineral growth. A highly fissile rock splits easily along the cleavage.".
- Q5455231 label "Fissility (geology)".
- Q5455231 depiction Muzeum_Złota_w_Złotoryi_fyllit_Panenska_Hůrka_21.07.2011_p.jpg.