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Geology; December 2002; v. 30; no. 12; p. 1087-1090; DOI: 10.1130/0091-7613(2002)030<1087:NVRPCA>2.0.CO;2
© 2002 Geological Society of America
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Nicaraguan volcanoes record paleoceanographic changes accompanying closure of the Panama gateway

Terry Plank1, Vaughn Balzer2 and Michael Carr3

1 Department of Earth Sciences, Boston University, Boston, Massachusetts 02215, USA, and Department of Geology, University of Kansas, Lawrence, Kansas 66044, USA
2 Department of Geology, University of Kansas, Lawrence, Kansas 66044, USA, and Department of Geology, Oregon State University, Corvallis, Oregon 97331, USA
3 Department of Geological Sciences, Rutgers University, Piscataway, New Jersey 08854, USA

A major oceanographic event preserved in the Cocos plate sedimentary column survived subduction and is recorded in the changing composition of Nicaraguan magmas. A uranium increase in these magmas since the latest Miocene (after 7 Ma) resulted from the "carbonate crash" at 10 Ma and the ensuing high organic carbon burial in the sediments. The response of the arc to this paleoceanographic event requires near steady-state sediment recycling at this margin since 20 Ma. This relative stability in sediment subduction invites one of the first attempts to balance sedimentary input and arc output across a subduction zone. Calculations based on Th indicate that as much as 75% of the sedimentary column was subducted beneath the arc. The Nicaraguan margin is one of the few places to observe such strong links between the oceans and the solid earth.

Key Words: Nicaragua • volcano • geochemistry • sediment • uranium




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