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Neotectonics of the Macquarie Ridge Complex, Australia-Pacific plate boundary

Neotectonics of the Macquarie Ridge Complex, Australia-Pacific plate boundary
Neotectonics of the Macquarie Ridge Complex, Australia-Pacific plate boundary
New marine geophysical data along the Macquarie Ridge Complex, the Australia-Pacific plate boundary south of New Zealand, illuminate regional neotectonics. We identify tectonic spreading fabric and fracture zones and precisely locate the Australia-Pacific plate boundary along the Macquarie Ridge Complex. We interpret a ?5–10 km wide Macquarie Fault Zone between the two plates along a bathymétrie high that extends nearly the entire length of the Australia-Pacific plate boundary south of New Zealand. We conclude that this is the active Australia-Pacific strike-slip plate boundary. Arcuate fracture zones become asymptotic as they approach the plate boundary. A broad zone of less intense deformation associated with the plate boundary extends ?50 km on either side of the Macquarie Fault Zone. Marine geophysical data suggest that distinct segments of the plate boundary have experienced convergence and strike-slip deformation, although teleseismic evidence overwhelmingly indicates strike-slip motion along the entire surveyed boundary today. The McDougall and southernmost Puysegur segments show no evidence for past underthrusting, whereas data from the Macquarie and Hjort segments strongly suggest past convergence. The present-day strike-slip plate boundary along the Macquarie Ridge Complex coincides with the relict spreading center responsible for Australia-Pacific crust in the region. Our conceptual model for the transition from seafloor spreading to strike-slip motion along the Macquarie Ridge Complex addresses the decreasing length of spreading center segments and spacing between fracture zones, as well as the arcuate bend of the fracture zones that become asymptotic to the current transform plate boundary.
0148-0227
13457-13480
Massell, C.G.
537ea5ad-98d4-4e21-8c42-bd05c7af9dcf
Coffin, M.F.
b8285650-5efd-4129-ae91-1cf3f5911e89
Mann, P.
46aa7b33-cb1c-417a-96c1-afeedc929aa0
Mosher, S.
5dd6d126-f515-44b4-99db-90bea3bb28c8
Frohlich, C.
8c9476ff-ae18-4266-ac86-46794edd275d
Schuur, C.L.
f801b18e-4a19-47dc-92c0-a164157ee242
Karner, G.
673c6c55-6702-4db5-b595-bb8b9f5e1a20
Ramsay, D.
2cc99884-dad0-4764-ad45-5514ceaac229
Lebrun, J-F.
f4f1c6a6-bc53-42ea-ba43-7b3b9ca16192
Massell, C.G.
537ea5ad-98d4-4e21-8c42-bd05c7af9dcf
Coffin, M.F.
b8285650-5efd-4129-ae91-1cf3f5911e89
Mann, P.
46aa7b33-cb1c-417a-96c1-afeedc929aa0
Mosher, S.
5dd6d126-f515-44b4-99db-90bea3bb28c8
Frohlich, C.
8c9476ff-ae18-4266-ac86-46794edd275d
Schuur, C.L.
f801b18e-4a19-47dc-92c0-a164157ee242
Karner, G.
673c6c55-6702-4db5-b595-bb8b9f5e1a20
Ramsay, D.
2cc99884-dad0-4764-ad45-5514ceaac229
Lebrun, J-F.
f4f1c6a6-bc53-42ea-ba43-7b3b9ca16192

Massell, C.G., Coffin, M.F., Mann, P., Mosher, S., Frohlich, C., Schuur, C.L., Karner, G., Ramsay, D. and Lebrun, J-F. (2000) Neotectonics of the Macquarie Ridge Complex, Australia-Pacific plate boundary. Journal of Geophysical Research, 105 (B6), 13457-13480.

Record type: Article

Abstract

New marine geophysical data along the Macquarie Ridge Complex, the Australia-Pacific plate boundary south of New Zealand, illuminate regional neotectonics. We identify tectonic spreading fabric and fracture zones and precisely locate the Australia-Pacific plate boundary along the Macquarie Ridge Complex. We interpret a ?5–10 km wide Macquarie Fault Zone between the two plates along a bathymétrie high that extends nearly the entire length of the Australia-Pacific plate boundary south of New Zealand. We conclude that this is the active Australia-Pacific strike-slip plate boundary. Arcuate fracture zones become asymptotic as they approach the plate boundary. A broad zone of less intense deformation associated with the plate boundary extends ?50 km on either side of the Macquarie Fault Zone. Marine geophysical data suggest that distinct segments of the plate boundary have experienced convergence and strike-slip deformation, although teleseismic evidence overwhelmingly indicates strike-slip motion along the entire surveyed boundary today. The McDougall and southernmost Puysegur segments show no evidence for past underthrusting, whereas data from the Macquarie and Hjort segments strongly suggest past convergence. The present-day strike-slip plate boundary along the Macquarie Ridge Complex coincides with the relict spreading center responsible for Australia-Pacific crust in the region. Our conceptual model for the transition from seafloor spreading to strike-slip motion along the Macquarie Ridge Complex addresses the decreasing length of spreading center segments and spacing between fracture zones, as well as the arcuate bend of the fracture zones that become asymptotic to the current transform plate boundary.

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Published date: 2000

Identifiers

Local EPrints ID: 52435
URI: http://eprints.soton.ac.uk/id/eprint/52435
ISSN: 0148-0227
PURE UUID: e9a81997-7566-48bb-8642-4259c41b894f

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Date deposited: 26 Jun 2008
Last modified: 22 Jul 2022 20:59

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Contributors

Author: C.G. Massell
Author: M.F. Coffin
Author: P. Mann
Author: S. Mosher
Author: C. Frohlich
Author: C.L. Schuur
Author: G. Karner
Author: D. Ramsay
Author: J-F. Lebrun

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