astro.wikisort.org - Meteorite

Search / Calendar

Impactite is rock created or modified by one or more impacts of a meteorite.[1][2] Impactites are considered metamorphic rock, because their source materials were modified by the heat and pressure of the impact.[3] On Earth, impactites consist primarily of modified terrestrial material, sometimes with pieces of the original meteorite.[3]

An example of impactite on Earth (from Monturaqui impact crater, Chile)
An example of impactite on Earth (from Monturaqui impact crater, Chile)

Creation


When a large meteorite hits a planet, it can radically deform the rocks and regolith that it hits. The heat, pressure, and shock of the impact changes these materials into impactite.[3] Only very massive impacts generate the heat and pressure needed to transform a rock, so impactites are created rarely.[3]


Characteristics


Impactite includes shock-metamorphosed target rocks, melts (suevites) and mixtures of the two, as well as sedimentary rocks with significant impact-derived components (shocked mineral grains, tektites, anomalous geochemical signatures, etc.). In June 2015, NASA reported that impact glass has been detected on the planet Mars. Such material may contain preserved signs of ancient life—if life existed.[4] Impactites are generally classified into three groups: shocked rocks, impact melt, and impact breccias.[2]


Shocked rock


Shocked rocks have been transformed by shock metamorphism caused by the impact. They include shatter cones and high-pressure minerals, for example coesite and stishovite.


Impact melts


When a meteor strikes a planet's surface, the energy released from the impact can melt rock and soil into a liquid. The liquid then cools and becomes an impact melt.[2] If the liquid cools and hardens quickly into a solid, impact glass forms before the atoms have time to arrange into a crystal lattice. Impact glass can be dark brown, almost black, and partly transparent.[5] Sometimes, the cooled liquid does form a crystal structure. In that case, it would still be considered an impact melt, but not an impact glass.[2]


Impact breccias


Impact breccia from the Kara impact structure in Russia
Impact breccia from the Kara impact structure in Russia

Breccia is "a rock consisting of angular fragments cemented together".[6] An impact breccia is formed when a meteor shatters a rock and then cements it back together. Some breccias contain impact melts.[3]


Examples of impactite


Alga crater on Mars is a possible site for preserved ancient life, after detection of an impact glass deposit.[4]
Alga crater on Mars is a possible site for preserved ancient life, after detection of an impact glass deposit.[4]

Impactite has been found, for example, at the following impact craters and structures:


See also



References


  1. Stöffler, D.; Grieve, R.A.F. (1994). "Classification and Nomenclature of Impact Metamorphic Rocks: A Proposal to the IUGS Subcommission on the Systematics of Metamorphic Rocks". Lunar and Planetary Science Conference: 1347. Bibcode:1994LPI....25.1347S.
  2. Schmid, Rolf; Fettes, Douglas; Harte, Ben; Davis, Eleutheria; Desmons, Jacqueline; Smulikowski, Witold; Sassi, Francesco; Brodie, Kate; Árkai, Péter (2007), Fettes, Douglas; Desmons, Jacqueline (eds.), "Classification and nomenclature scheme", Metamorphic Rocks, Cambridge University Press, pp. 3–110, doi:10.1017/cbo9780511628917.003, ISBN 978-0-511-62891-7
  3. "Impactites: Impact Breccia, Tektites, Moldavites, Shattercones". geology.com. Retrieved 2020-06-10.
  4. Staff (8 June 2015). "PIA19673: Spectral Signals Indicating Impact Glass on Mars". NASA. Retrieved 8 June 2015.
  5. Temming, Maria. "Exotic Glass Could Help Unravel Mysteries of Mars". Scientific American. Retrieved 2015-06-15.
  6. Holland, Stuart S. (1976). Landforms of British Columbia: A Physiographic Outline (PDF). British Columbia, Canada. p. 127.
  7. Meteor Crater Bomblets




На других языках


- [en] Impactite

[ru] Импактиты

Импактиты (от англ. impact — «столкновение», «удар») — космогенные горные породы, образовавшиеся в результате ударно-взрывного (импактного) породообразования и ударного метаморфизма при столкновении крупных метеоритов с поверхностью Земли. Локализованы в астроблемах. При образовании импактитов показатели давления и температуры достигают десятков гигапаскалей и 2000—3000°С соответственно, а скорости изменения этих параметров превышают скорости их эволюции в других типах породообразующих процессов на несколько порядков.



Текст в блоке "Читать" взят с сайта "Википедия" и доступен по лицензии Creative Commons Attribution-ShareAlike; в отдельных случаях могут действовать дополнительные условия.

Другой контент может иметь иную лицензию. Перед использованием материалов сайта WikiSort.org внимательно изучите правила лицензирования конкретных элементов наполнения сайта.

2019-2025
WikiSort.org - проект по пересортировке и дополнению контента Википедии