Structure of a fossil ridge–transform intersection in the Troodos ophiolite


RECENT palaeomagnetic studies of sheeted dykes adjacent to the east-west trending Southern Troodos transform fault of Cyprus have demonstrated significant clockwise block rotations, which are most easily interpreted as being due to drag induced by dextral strike-slip faulting along the transform1–6. We show here that such rotations have not occurred along… (More)
DOI: 10.1038/348717a0


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