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Earliest Eocene (53 Ma) convergence in the Southwest Pacific: evidence from pre-obduction dikes in the ophiolite of New Caledonia

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Cluzel, D, Meffre, S, Maurizot, P and Crawford, AJ 2006 , 'Earliest Eocene (53 Ma) convergence in the Southwest Pacific: evidence from pre-obduction dikes in the ophiolite of New Caledonia' , Terra Nova, vol. 18, No. 6 , pp. 395-402 , doi: 10.1111/j.1365-3121.2006.00704.x.

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Abstract

Uncertainty about the timing and location of the initiation of
convergence in the western and south-western Pacific greatly
hinders accurate plate tectonic reconstructions of subduction
systems in that area. The chemistry and age of dikes intruding
mantle peridotite in the ophiolite of New Caledonia infer that
subduction-related magmatism began before 53 Ma. These new
results infer that obduction in the south-west Pacific is
unrelated to the reorientation of the Pacific plate motion that
occurred c. 43 Ma and confirm new interpretations showing
that changes in mantle flow, hotspot and plate motion may
have occurred as soon as late Paleocene or early Eocene.

Item Type: Article
Authors/Creators:Cluzel, D and Meffre, S and Maurizot, P and Crawford, AJ
Journal or Publication Title: Terra Nova
ISSN: 1365-3121
DOI / ID Number: 10.1111/j.1365-3121.2006.00704.x
Additional Information:

http://www.blackwell-synergy.com/doi/abs/10.1111/j.1365-3121.2006.00704.x

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