Origin of a Giant Event Deposit in Northwestern Cuba and Its Relation to K/T Boundary Impact

Details Origin of a Giant Event Deposit in Northwestern Cuba and Its Relation to K/T Boundary Impact Origin of a Giant Event Deposit in Northwestern Cuba and Its Relation to K/T Boundary Impact

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1534t&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1534

Physics

Scientific paper

We investigated the Penalver Formation in northwestern Cuba, which is a
<180 m thick, normal-graded calcareous clastic deposit. This
formation must have been formed by a grain flow and huge tsunami waves
caused by the K/T boundary impact.

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