Volcanoes of the southwestern extension of the active Mariana island arc: New swath-mapping and geochemical studies |
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| Authors: | P FRYER H SUJIMOTO M SEKINE L E JOHNSON J KASAHARA H MASUDA T GAMO T ISHII M ARIYOSHI & K FUJIOKA |
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| Institution: | School of Ocean and Earth Science and Technology, Hawaii Institute of Geophysics and Planetology, 2525 Correa Road, Honolulu, Hawaii 96822, Japan,;Ocean Research Institute University of Tokyo, 1–15–1, Minamidai, Nakano-ku, Tokyo 164, Japan,;Ocean Research Institute University of Tokyo, 1–1–1, Yayoi, Bunkyo-ku, Tokyo 113, Japan,;MBARI (Monterey Bay Aquarium Research Institute), PO Box 628, Moss Landing, CA 95039, USA,;Faculty of Science, Osaka City University, Sugimoto, Sumiyoshi-ku, Osaka 558, Japan,;Deep Sea Research Department, JAMSTEC 2–15 Natsushima-cho, Yokosuka, Kanagawa 237, Japan |
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| Abstract: | Until recently it was thought that the volcanoes of the Mariana island arc of the western Pacific terminated at Tracey Seamount at ∼ 14°N immediately west of Guam. Sea floor mapping in 1995 shows a series of large volcanic seamounts stretching westward for nearly 300 km beyond that point. The morphology, spacing, and composition of those sampled are consistent with their having formed as a consequence of eruption of suprasubduction zone arc magmas. The relationships of the volcanoes to the tectonic processes of subduction of the Pacific plate beneath the southern portion of the Mariana convergent plate margin are becoming increasingly clear as new bathymetry and geochemical data are amassed. The volcanoes along this trend that lie closest to Guam are forming where the center of active extension in the back-arc basin intersects the line of arc volcanoes. They develop well-defined rifts that are parallel to rift structures along the extension center, whereas volcanoes of the spreading axis to the north are smaller than the frontal arc volcanoes and tend to form along lineaments. Compositions of lavas from these intersection volcanoes bear some similarities to back-arc basin basalt, but are on the whole well within the range of compositions for Mariana island arc lavas. The Pacific plate subducts nearly orthogonal to the strike of the trench along the southern part of the Mariana system and the distance to the arc line from the trench axis is only ∼ 150 km. Several deep fault-controlled canyons on the inner slope of the southern Mariana trench indicate an enhanced tectonic extension of this plate margin. The presence of these active arc volcanoes and the existence of the orthogonal normal faulting along the southern Mariana forearc supports a model of radial extension for formation of the Mariana Trough, a model previously dismissed because of the lack of evidence of these two major geological features. |
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| Keywords: | basalt convergent margin forearc island arc Mariana side-scan sonar subduction volcanism |
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