Movatterモバイル変換


[0]ホーム

URL:


Jump to content
WikipediaThe Free Encyclopedia
Search

Cryptoexplosion

From Wikipedia, the free encyclopedia
Type of crater

Ingeology, acryptoexplosion structure (orcryptovolcanic structure) is an explosion of unknown cause. The term is now largely obsolete. It was once commonly used to describe sites where there was geological evidence of a large-scale explosion within theEarth's crust, but no definitive evidence for the cause such as normalvolcanic rocks. These sites are usually circular with signs of anomalous rock deformation contrasting with the surrounding region, and often showing evidence that crustal material had been uplifted and/or blown outwards. The assumption was that some unusual form of volcanism, or a gas explosion originating within the crust, was the cause. The use of the term went away with the rise of the science of impact crater recognition in the late 20th century. Most structures described as cryptoexplosions turned out to be erodedimpact craters, caused by the impact ofmeteorites. Today geologists discount former cryptoexplosion theories.[1]

See also

[edit]

References

[edit]
  1. ^French, Bevan M (1998).Traces of Catastrophe: A Handbook of Shock-Metamorphic Effects in Terrestrial Meteorite Impact Structures(PDF). LPI Contribution No. 954.Houston:Lunar and Planetary Institute. p. 120.ASIN B0006R1XF8.Bibcode:1998trca.book.....F.OCLC 40770730. Retrieved2011-09-02.
Types
Volcanic rocks
Lists and groups
Lists

Confirmed
≥20 km diameter
Topics
Research
Authority control databases: NationalEdit this at Wikidata


Stub icon

This article about animpact crater onEarth is astub. You can help Wikipedia byexpanding it.

Retrieved from "https://en.wikipedia.org/w/index.php?title=Cryptoexplosion&oldid=1232287459"
Categories:
Hidden categories:

[8]ページ先頭

©2009-2025 Movatter.jp