First manned submersible dives on the East Pacific Rise at 21°N (project RITA): General results |
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| Authors: | J Francheteau H D Needham P Choukroune T Juteau M Séguret R D Ballard P J Fox W R Normark A Carranza D Cordoba J Guerrero C Rangin Cyamex Scientific Team |
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| Institution: | (1) CNEXO, France;(2) Université de Rennes, France;(3) Université de Strasbourg, France;(4) Université de Montpellier, France;(5) Woods Hole Oceanographic Institution, USA;(6) SUNY at Albany, USA;(7) USGS Menlo Park, USA;(8) UNAM, Mexico;(9) UNAM, Mexico;(10) Present address: Université de Paris 6, Paris, France |
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| Abstract: | A submersible study has been conducted in February–March 1978 at the axis of the East Pacific Rise near 21°N. The expedition CYAMEX, the first submersible program to be conducted on the East Pacific Rise, is part of the French-American-Mexican project RITA (Rivera-Tamayo), a 3-year study devoted to detailed geological and geophysical investigations of the East Pacific Rise Crest. On the basis of the 15 dives made by CYANA in the axial area of the Rise, a morphological and tectonic zonation can be established for this moderately-fast spreading center. A narrow, 0.6 to 1.2 km wide zone of extrusion (zone 1), dominated by young lava flows, is flanked by a highly fissured and faulted zone of extension (zone 2) with a width of 1 to 2 km. Further out, zone 3 is dominated by outward tilted blocks bounded by inward-facing fault scarps. Active or recent faults extend up to 12 km from the axis of extrusion of the East Pacific Rise. This represents the first determination from direct field evidence of the width of active tectonism associated with an accreting plate boundary. Massive sulfide deposits, made principally of zinc, copper and iron, were found close to the axis of the Rise. Other signs of the intense hydrothermal activity included the discovery of benthic fauna of gian size similar to that found at the axis of the Galapagos Rift. We emphasize the cyclic character of the volcanicity. The main characteristics of the geology of this segment of the East Pacific Rise can be explained by the thermal structure at depth below this moderately-fast spreading center. The geological observations are compatible with the existence of a shallow magma reservoir centered at the axis of the Rise with a half-width of the order of 10 km. |
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