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Science 18 August 1967: Vol. 157. no. 3790, pp. 801 - 803 DOI: 10.1126/science.157.3790.801
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Articles
Andesitic Volcanism and Seismicity around the Pacific
William R. Dickinson 1 and
Trevor Hatherton 2
1 School of Earth Sciences, Stanford University, Stanford, California
2 Geophysics Division, Department of Scientific and Industrial Research, Wellington, New Zealand
Circum-Pacific andesites, with associated basalts and dacites, are erupted from linear island arcs and marginal continental ranges whose ocean-side borders coincide approximately with the continent-side boundaries of belts of shallow seismicity that parallel adjacent trenches. The lines of active volcanoes stand above elongate subcrustal regions delineated by the intersection of inclined Benioff seismic zones and the subhorizontal Gutenberg low-velocity zone. Close correlation between content of potash in erupted lavas and vertical depth to the Benioff zone suggests that andesitic volcanism has its origins in the mantle where magmas are generated by events associated with earthquakes of intermediate focal depth.
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