The Manila Trench - West Taiwan Foldbelt: a flipped subduction zone
The Manila Trench-West Taiwan Foldbelt is an anomalous west-facing island arc segment of the western Pacific. It is postulated to be a young, east-dipping subduction zone which flipped in Pliocene time from a former west-dipping position on the east side of Luzon and Taiwan, where it probably formed...
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Geological Society of Malaysia
1973
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