Pacifica and new zealand: proposed eastern elements in gondwanaland's history


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ABSTRACT The origin of the sediments of the Canterbury Suite to the east of the Alpine Fault in New Zealand, cannot have derived from Marie Byrd Land before or during the breaking up of


Gondwanaland. It is argued that the sediments may have derived from the lost continent of Pacifica, which is supposed to have separated from Gondwanaland in the late Palaeozoic. Such a


mechanism can also account for the recurrence of similar quartzo-feldspathic sediments in California and thus of the Mesozoic dolerites and basalts in southern Africa, Antarctica and


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_Earth planet. Sci. Lett._ 36, 77–84 (1977). Article  ADS  Google Scholar  Download references AUTHOR INFORMATION AUTHORS AND AFFILIATIONS * Earth Sciences and Antarctic Research Unit,


University of Waikato, Hamilton, New Zealand P. J. J. Kamp Authors * P. J. J. Kamp View author publications You can also search for this author inPubMed Google Scholar RIGHTS AND PERMISSIONS


Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE Kamp, P. Pacifica and New Zealand: proposed eastern elements in Gondwanaland's history. _Nature_ 288, 659–664 (1980).


https://doi.org/10.1038/288659a0 Download citation * Received: 05 August 1980 * Accepted: 22 October 1980 * Issue Date: 18 December 1980 * DOI: https://doi.org/10.1038/288659a0 SHARE THIS


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