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Magmatic evolution of Pacaya and Cerro Chiquito volcanological complex, Guatemala

Bulletin of Volcanology, 1992
Four major phases are distinguished during the building of the Pacaya volcanological complex (Guatemala): (1) the ‘ancestral volcano’, now much eroded, covered by younger deposits and battered by faulting and landslides; (2) the initial cone made up of large lava flows and dated at about 0.5 Ma; (3) andesito-dacitic domes (Cerro Chiquito dome and ...
Jacques-Marie Bardintzeff   +1 more
openaire   +1 more source

Registration of ‘Rojo Chiquito’ Small Red Dry Bean

Crop Science, 2002
A.N. Hang   +3 more
openaire   +1 more source

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