Skip to main content

Impact Melt Rock

Encyclopedia of Astrobiology
  • 210 Accesses

Definition

An impact melt rock is a type of rock typically found in impact structures. It is an impactite consisting of a mixture of solid and melt fragments all derived from the target rock, floating in a glassy, microcrystalline, or recrystallized matrix. The solid fragments may contain shocked minerals. An impact melt rock results from the cooling of the melt pool that formed within a crater because of the high temperature and pressure generated during the impact. The largest craters such as Sudbury (Ontario, Canada), Chicxulub (Mexico), Popigai (Siberia), or Manicouagan (Québec, Canada) contain a very large volume of impact melt. In the case of Sudbury, it also hosts important ore deposits of nickel.

See Also

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Institutional subscriptions

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Philippe Claeys .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2014 Springer-Verlag Berlin Heidelberg

About this entry

Cite this entry

Claeys, P. (2014). Impact Melt Rock. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_779-3

Download citation

  • DOI: https://doi.org/10.1007/978-3-642-27833-4_779-3

  • Received:

  • Accepted:

  • Published:

  • Publisher Name: Springer, Berlin, Heidelberg

  • Online ISBN: 978-3-642-27833-4

  • eBook Packages: Springer Reference Physics and AstronomyReference Module Physical and Materials ScienceReference Module Chemistry, Materials and Physics

Publish with us

Policies and ethics

Chapter history

  1. Latest

    Impact Melt Rock
    Published:
    01 May 2022

    DOI: https://doi.org/10.1007/978-3-642-27833-4_779-4

  2. Original

    Impact Melt Rock
    Published:
    30 April 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_779-3