Regional implications of U/Pb SHRIMP age constraints on the tectonic evolution of New Caledonia

Author:

Aitchison J.C,Ireland T.R,Clarke G.L,Cluzel D,Davis A.M,Meffre S

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference47 articles.

1. Provenance of Permian–Triassic and Ordovician metagraywacke terranes in New Zealand: evidence from 40Ar/39Ar dating of detrital micas;Adams;Geol. Soc. Am. Bull.,1998

2. Eocene arc–continent collision in New Caledonia and implications for regional Southwest Pacific tectonic evolution;Aitchison;Geology,1995

3. Probable Precambrian detrital zircons in New Caledonia and southwest Pacific continental structure;Aronson;Geol. Soc. Am. Bull.,1971

4. Ballance, P.F., Campbell, J.D., 1993. The Murihiku arc-related basin of New Zealand (Triassic–Jurassic). In: Ballance, P.F. (Ed.), South Pacific Sedimentary Basins. Sedimentary Basins of the World. Elsevier, Amsterdam, pp. 21–33.

5. Benson, W.N., 1928. The Mesozoic rocks of New Caledonia and their relation to those of New Zealand. Third Pan Pacific Science Congress, Tokyo, pp. 1701–1703.

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