The Semail Ophiolite in the Sultanate of Oman, and the Bay of Islands and St. Anthony Ophiolite Complexes in western Newfoundland show a similar multistage history of ophiolite obduction. This involved both intra-oceanic detachment of the ophiolite slabs and their emplacement onto the continental margin. Structural relations within these examples clearly indicate a complex scenario of assembly which involved initial delamination between the drift and rift facies segments of the continental margin sequence followed by major break-back (out-of-sequence) thrusting. -from Authors
CITATION STYLE
Cawood, P. A. (1991). Process of ophiolite emplacement in Oman and Newfoundland. Ophiolite Genesis and Evolution of the Oceanic Lithosphere. Proc. Conference, Muscat, 1990, 501–516. https://doi.org/10.1007/978-94-011-3358-6_25
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