Shock-induced microdeformations in quartz and other mineralogical indications of an impact event at the Cretaceous-Tertiary boundary.

Details Shock-induced microdeformations in quartz and other mineralogical indications of an impact event at the Cretaceous-Tertiary boundary. Shock-induced microdeformations in quartz and other mineralogical indications of an impact event at the Cretaceous-Tertiary boundary.

Jan 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990tectp.171..359b&link_type=abstract

Tectonophysics, Vol. 171, No. 1-4, p. 359 - 372

Physics

14

Earth: Impact Phenomena

Scientific paper

The event terminating the Cretaceous period and the Mesozoic era caused massive extinctions of flora and fauna worldwide. Theories of the nature of this event can be classed as endogenic (volcanic, climatic, etc.) or exogenic (extraterrestrial causes). All features of the boundary clay are uniquely associated with impact, and cannot have been formed by volcanic or other terrestrial processes.

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