Abstract
Six holes were drilled at three sites in the fore-arc region. A major stratigraphic inversion is present in Hole 541 at a depth of 276m below the seafloor, thought to be a reverse fault formed by imbricate underthrusting during the formation of an accretionary prism at the active margin.-from Author
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CITATION STYLE
APA
Bergen, J. A. (1984). Calcareous nannoplankton from Deep Sea Drilling Project Leg 78A: evidence for imbricate underthrusting at the Lesser Antillian active margin. Initial Reports, DSDP, Leg 78A, from San Juan, Puerto Rico, 411–445. https://doi.org/10.2973/dsdp.proc.78a.120.1984
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