2003 Seattle Annual Meeting (November 2–5, 2003)

Paper No. 11
Presentation Time: 4:15 PM


WALKER, James A.1, MICKELSON, J. Erik1, THOMAS, Rebecca B.2, PATINO, Lina C.3, CAMERON, Barry I.4 and EDWARDS, R. Lawrence5, (1)Northern Illinois Univ, Dept Geology & Environmental Geosciences, De Kalb, IL 60115-2854, (2)Dept Geology and Geophysics, Univ of Minnesota, Minneapolis, MN 55455, (3)Michigan State Univ, 206 Natural Science, East Lansing, MI 48824-1115, (4)Dept of Geosciences, Univ of Wisconsin-Milwaukee, Milwaukee, WI 53201, (5)Department of Geology & Geophysics, Univ of Minesota, Minneapolis, MN 55455, georock2@juno.com

Guatemalan lavas exhibit systematic along-arc variations in U-series isotope data. Lavas from the northwestern part of the volcanic front have (230Th/238U) < 1. In contrast, lavas erupted in central Guatemala, from Fuego volcano to cinder cones immediately east of Pacaya volcano, have (230Th/238U) > 1. Excesses in (238U) then reappear in lavas from southeastern Guatemala, including a lava erupted in the Ipala Graben over 50 km behind the front. All of the (230Th/232Th) ratios of Guatemalan lavas are similar to values found in Costa Rica at the opposite end of the volcanic chain. A dacitic lava erupted in 1818 from Cerro Quemado, in the northwestern part of Guatemala, has only a slight (238U) excess, suggesting it suffered prolonged differentiation and/or crustal contamination. A subset of the mafic lavas has elevated slab signatures. The (230Th/238U) ratios of the mafic lavas show positive correlations with Th/Nb and U/La. The data suggest that two particular processes may be crucial in explaining the observed geographic variations in (230Th/238U) along the Guatemalan volcanic front: sediment melting in the subducting Cocos plate and decompression melting in the overlying mantle wedge.