Difference between revisions of "Fissility"

From CAMEO
Jump to navigation Jump to search
(username removed)
Line 1: Line 1:
 
== Description ==
 
== Description ==
  
Property of certain rocks to easily split into regular thin sheets.  Fissility occurs because the platy [http://cameo.mfa.org/materials/fullrecord.asp?name=phyllosilicate phyllosilicate] grains have been preferentially aligned to form a layered structure.  Examples of rocks that exhibit fissility are [http://cameo.mfa.org/materials/fullrecord.asp?name=shale shale], and [http://cameo.mfa.org/materials/fullrecord.asp?name=slate slate].
+
Property of certain rocks to easily split into regular thin sheets.  Fissility occurs because the platy [[phyllosilicate]] grains have been preferentially aligned to form a layered structure.  Examples of rocks that exhibit fissility are [[shale]], and [[slate]].
  
 
== Synonyms and Related Terms ==
 
== Synonyms and Related Terms ==

Revision as of 11:33, 15 January 2014

Description

Property of certain rocks to easily split into regular thin sheets. Fissility occurs because the platy Phyllosilicate grains have been preferentially aligned to form a layered structure. Examples of rocks that exhibit fissility are Shale, and Slate.

Synonyms and Related Terms

fissilidade (Port.)

Authority

  • Submitted information Comment: José Delgado Rodrigues, LNEC, 2009

Retrieved from "https://cameo.mfa.org/index.php?title=Fissility&oldid=44464"