The Chimborazo sector collapse and debris avalanche: Deposit characteristics as evidence of emplacement mechanisms

Article

Abstract: Chimborazo is a Late Pleistocene to Holocene stratovolcano located at the southwest end of the main

Palabras claves:

block facies, CHIMBORAZO, debris avalanche deposit, emplacement, mixed facies, structures

Autores:

Alcaraz S., Claude Robin, D. Barba, Julien Bernard, Leyrit H., Pablo Samaniego Ponce, Van Wyk de Vries B.

Fuentes:

scopus