Igneous Rocks Classification Quiz
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Igneous Rocks Classification Quiz

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Questions and Answers

What characterizes metaluminous rocks in terms of aluminum content?

  • They have a positive aluminum index (A.I.) (correct)
  • They contain only sodic pyroxenes
  • They have a negative aluminum index (A.I.)
  • They are classified as SiO₂-saturated (correct)
  • Which minerals are characteristic of SiO₂-undersaturated metaluminous rocks?

  • Nepheline and ferric amphiboles
  • Nepheline and calcic pyroxenes (correct)
  • Quartz and sodic pyroxenes
  • Leucite and quartz
  • What does a negative aluminum index (A.I.) indicate about a rock?

  • It must be SiO₂-saturated
  • It belongs to the peralkaline category (correct)
  • It is metaluminous in classification
  • It contains only quartz
  • Which minerals would you expect to find in SiO₂-saturated peralkaline rocks?

    <p>Quartz and sodic pyroxenes</p> Signup and view all the answers

    How does the presence of trace elements relate to igneous rock classification?

    <p>They assist in further characterizing specific rock types</p> Signup and view all the answers

    Study Notes

    Feldspathoid-Silica Saturation Index (FSSI)

    • The FSSI classifies igneous rocks based on the presence of certain minerals.
    • Metaluminous rocks have a positive aluminum (Al) content.
    • Peralkaline rocks have a negative aluminum (Al) content.
    • Silica-undersaturated rocks contain minerals like nepheline, calcic or sodic pyroxenes, and amphiboles.
    • Silica-saturated rocks contain minerals like quartz, ferric, magnessian, or calcic pyroxenes, and amphiboles.
    • Quartz-saturated rocks have an excess of quartz over leucite and nepheline.
    • Silica-undersaturated rocks have a negative amount of quartz over leucite and nepheline.

    Trace Elements

    • Trace elements are used to characterize igneous rocks.

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    Description

    Test your knowledge on the Feldspathoid-Silica Saturation Index (FSSI) and how it classifies igneous rocks. This quiz covers the distinctions between metaluminous, peralkaline, and various types of silica-saturation in rocks, as well as the role of trace elements in characterization.

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