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Introduction

  • Roger Hekinian
  • Jean-Louis Cheminée
  • Peter Stoffers

Abstract

Intraplate volcanism occurs in both submarine and subaerial regions on the Earth’s surface. However, most of the magmatic activity responsible for the construction of the Earth’s volcanic structures takes place under the sea in oceanic basins and along spreading centers. The divergent plate boundaries (Mid-Ocean Ridges) and back-arcs are relatively straight and structurally continuous features, making them easier to investigate than the more scattered and dispersed intraplate volcanic provinces within the oceanic basins.

Keywords

Mantle Plume Spreading Center Debris Avalanche Volcanic Chain Intraplate Volcanism 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag Berlin Heidelberg 2004

Authors and Affiliations

  • Roger Hekinian
  • Jean-Louis Cheminée
  • Peter Stoffers

There are no affiliations available

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