Geochemical trends of sequential lava flows from Meseta volcano, Guatemala

• Published in: Journal of volcanology and geothermal research Vol. 78; no. 3; pp. 221 - 237
• Main Authors: Chesner, Craig A., Halsor, Sid P.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-09-1997
• Subjects: magmatic evolution; Meseta volcano; sector collapse; sequential lavas; temporal geochemical trends; magmatic evolution; Meseta volcano; sequential lavas; sector collapse; temporal geochemical trends
• ISSN: 0377-0273; 1872-6097
• DOI: 10.1016/S0377-0273(97)00014-0

The Meseta and Fuego volcanoes closely overlap and collectively are known as the Fuego Volcanic Complex. Historic activity occurs exclusively at Fuego, the southern center, and consists of high-Al basalts. Meseta, the inactive northern center, is predominantly composed of basaltic andesites with minor basalt and andesite. A thick sequence of lava flows and dikes is exposed by a steep collapse escarpment on the east flank of Meseta. The upper 75% of the sequence was sampled from three interfingering stratigraphic sections consisting of 27, 10 and 4 lavas, respectively. Temporal geochemical trends of each section indicates a complex evolutionary history. A major trend toward more evolved compositions upward in the section is consistent with crystal fractionation. This trend is sharply interrupted by the youngest lavas which become distinctly more mafic in composition. Magma mixing is apparently the dominant magmatic evolution process that generated these lavas. The two trends have distinct Sr signatures that suggest a change in parental magma compositions. This abrupt change in composition is interpreted to signal high input rates of mafic magma into the subvolcanic magma chamber. These changes eventually led to sector collapse of Meseta volcano and deposition of the Escuintla debris avalanche. Eruptive activity then migrated to the Fuego volcano where historic activity is similar to that of Meseta immediately prior to its collapse.