Petrology, Geochemistry, and Ages of Lavas from Northwest Hawaiian Ridge Volcanoes
Downloaded from specialpapers.gsapubs.org on June 17, 2015 The Geological Society of America Special Paper 511 2015 Petrology, geochemistry, and ages of lavas from Northwest Hawaiian Ridge volcanoes Michael O. Garcia Department of Geology and Geophysics, SOEST, University of Hawai‘i at Mānoa, Honolulu, Hawai‘i 96822, USA John R. Smith Hawai‘i Undersea Research Laboratory, SOEST, University of Hawai‘i at Mānoa, Honolulu, Hawai‘i 96822, USA Jonathan P. Tree Department of Geology and Geophysics, SOEST, University of Hawai‘i at Mānoa, Honolulu, Hawai‘i 96822, USA Dominique Weis Lauren Harrison Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T1Z4, Canada Brian R. Jicha Department of Geoscience, University of Wisconsin-Madison, Madison, Wisconsin 53706, USA ABSTRACT The Northwest Hawaiian Ridge is a classic example of a large igneous province. The morphology and geology of the ridge is poorly characterized, although it consti- tutes the longest segment (~47%) of the Hawaiian-Emperor Chain. Here we present a new bathymetric compilation, petrographic and X-ray fl uorescence (XRF) data for lavas from 12 volcanoes along the Northwest Hawaiian Ridge, and review literature data for the age and isotopic variation of the ridge. The bathymetric compilation revealed that the Northwest Hawaiian Ridge consists of at least 51 volcanoes. The 45 new XRF analyses show that the Northwest Hawaiian Ridge contains tholeiitic and alkalic lavas with compositions typical of lavas from the Hawaiian Islands. The absolute ages and duration of volcanism of individual Northwest Hawaiian Ridge volcanoes are poorly known, with modern 40Ar/39Ar ages for only 10 volcanoes, mostly near the bend in the chain.
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