Abstract
A feature common to the history of all the oceans has been the extension of the oceanic crust as a result of the repeated introduction of new material along the mid-oceanic ridges. In the young oceans widening of the ocean basins themselves since Mesozoic times has been made possible by the lateral drift of the adjacent continental fragments: oceanic and continental crustal masses have moved together as composite crustal plates. There is a fundamental contrast between the tectonic setting of these widening oceans and that of shrinking oceans, such as the Pacific, which are dealt with in Chapter 10. The former are coupled to the bordering continents; the latter are detached from the bordering continents along the world-wide system of mobile belts at which the surplus crustal material is returned to depth (Fig. 9.1).
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© 1975 The Estate of the late H. H. Read and Janet Watson
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Read, H.H., Watson, J. (1975). The New Ocean Basins. In: Introduction to Geology. Palgrave, London. https://doi.org/10.1007/978-1-349-15613-9_9
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