New Zealand Journal of Geology and Geophysics abstracts

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Tectonic reconstructions of New Zealand: 40 Ma to the Present

PETER R. KING

Institute of Geological & Nuclear Sciences
P.O. Box 30 368
Lower Hutt, New Zealand
email: p.king@gns.cri.nz

Abstract  Reconstructions of the New Zealand subcontinent from 40 Ma to the Present are presented. Assumptions that have constrained the model include: semi-straight initial alignment of basement terranes and markers; Australian plate fixed; onset of Emerald Basin spreading at c. 45 Ma; and Pacific plate subduction north of New Zealand from c. 30 Ma. Five independent, rigid, crustal blocks are employed, including: Northland-Taranaki-western South Island (combined), East Coast (North Island), east Nelson (Marlborough Sounds), eastern South Island, and Fiordland.

At 40 Ma the Pacific/Australian rotation pole was located close to or within the Wanganui region. A proto-plate boundary zone was propagating through western New Zealand, as an incipient link between Emerald Basin spreading in the south and subduction in the northwest. Lateral offset on the Alpine Fault was initiated by c. 23-22 Ma, mainly as an effect of changing subduction kinematics and increasing relative motion of the Australian and Pacific plates in the central New Zealand region. Extension in the south became increasingly oblique, whereas areas north of the Alpine Fault were affected by nearorthogonal compression. From c. 23 Ma to the Present, the foci of contraction, extension, and arc volcanism in centralwestern New Zealand have migrated southwards, in response to progressive changes in the location, orientation, inclination, and kinematics of the subducted Pacific plate.

Keywords  tectonic reconstructions; New Zealand; Cenozoic; Alpine Fault; Australia-Pacific plate boundary

New Zealand Journal of Geology & Geophysics, 2000, Vol. 43: 611-638

0028-8306/00/4304-0611 $7.00/0 (c) The Royal Society of New Zealand 2000

PDF file of entire paper: medium quality (2921K); (scanned from paper original: notes about this process)

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