Difference between revisions of "Leucocratic rock"

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== Description ==
 
== Description ==
  
[http://cameo.mfa.org/materials/fullrecord.asp?name=Igneous Igneous] rock containing 65 to 95% of [http://cameo.mfa.org/materials/fullrecord.asp?name=felsic%20minerals felsic minerals], such as feldspathoids ([http://cameo.mfa.org/materials/fullrecord.asp?name=nepheline nepheline] and [http://cameo.mfa.org/materials/fullrecord.asp?name=leucite leucite]), [http://cameo.mfa.org/materials/fullrecord.asp?name=muscovite muscovite], and [http://cameo.mfa.org/materials/fullrecord.asp?name=corundum corundum]. Because felsic minerals lack iron and magnesium, they are generally light in color and consequently are referred to as leucocratic.
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[[Igneous]] rock containing 65 to 95% of [[felsic minerals]], such as feldspathoids ([[nepheline]] and [[leucite]]), [[muscovite]], and [[corundum]]. Because felsic minerals lack iron and magnesium, they are generally light in color and consequently are referred to as leucocratic.
  
 
== Synonyms and Related Terms ==
 
== Synonyms and Related Terms ==

Revision as of 13:30, 21 January 2014

Description

Igneous rock containing 65 to 95% of Felsic minerals, such as feldspathoids (Nepheline and Leucite), Muscovite, and Corundum. Because felsic minerals lack iron and magnesium, they are generally light in color and consequently are referred to as leucocratic.

Synonyms and Related Terms

rocha leucocrática (Port.)

Authority

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

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