Abstract
ABSTRACT: In this paper we present sedimentological, chemical and geochronological data on a pyroclastic sequence deposited at Chichontepeque Volcano (El Salvador) during a caldera-forming Plinian phase. Granulometric analyses and width distribution patterns of airfall pyroclastics showed that these are the result of at least two eruptions, the oldest being the more complete. The Basal Fall, which marks the beginning of the Plinian eruption, shows the typical features of Plinian air-fall deposits. Chemical trends mirror roughly a downward tapping from a zoned magma chamber; inside each fall unit crys- tal fractionation trends can be recognized. 39Ar/40Ar dating of lavas underlying and overlying the pyroclastic sequence show that the Plinian phase occurred between 0.59 ±0.09 and 0.55±0.04 Ma before present.
Cite
CITATION STYLE
Aiuppa., A., Rotolo, S. G., & Villa, I. M. (2013). Stratigraphy, geochemistry and geochronology of a Quaternary pyroclastic sequence of the Chichontepec volcano, El Salvador. Revista Geológica de América Central, (22). https://doi.org/10.15517/rgac.v0i22.8588
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