Fig. 2. —Sketch map showing the Alpine Fault and pre-Cretaceous rocks of the South Island, reproduced from Wellman (1952). The 300-mile lateral shift is based on the correspondence of regional sequences on opposite sides of the Alpine Fault in the north and south of the Island.
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Transactions of the Royal Society of New Zealand : Geology, Volume 2, Issue 7, 7 August 1963, Page 107
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46Fig. 2.—Sketch map showing the Alpine Fault and pre-Cretaceous rocks of the South Island, reproduced from Wellman (1952). The 300-mile lateral shift is based on the correspondence of regional sequences on opposite sides of the Alpine Fault in the north and south of the Island. Transactions of the Royal Society of New Zealand : Geology, Volume 2, Issue 7, 7 August 1963, Page 107
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