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Magmatism during Gondwana break-up: new geochronological data from Westland, New Zealand

  • Newly determined Late Cretaceous Ar-40/Ar-39 ages on megacrystic kaersutite from four lamprophyre dikes, and a U-Pb zircon age on a trachyte, from central and north Westland (New Zealand) are presented. These ages suggest that the intrusion of mafic dikes (88-86 and 69 Ma) was not necessarily restricted to the previously established narrow age range of 80-92 Ma. The younger lamprophyre and trachyte dikes (c. 68-70 Ma) imply that tensional stresses in the Western Province were either renewed at this time, or that extension and related magmatism continued during opening of the Tasman Sea. Extension-related magmatism in the region not only preceded Tasman seafloor spreading initiation (starting at c. 83 Ma, lasting to c. 53 Ma), but may have sporadically continued for up to 15 Ma after continental break-up.

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Author details:Q. H. A. Van der Meer, James M. Scott, T. E. Waight, Masafumi SudoORCiDGND, A. Schersten, Alan F. Cooper, Terry L. Spell
DOI:https://doi.org/10.1080/00288306.2013.826699
ISSN:0028-8306
ISSN:1175-8791
Title of parent work (English):New Zealand journal of geology and geophysics : an international journal of pacific rim geosciences
Publisher:Routledge, Taylor & Francis Group
Place of publishing:Abingdon
Publication type:Article
Language:English
Year of first publication:2013
Publication year:2013
Release date:2017/03/26
Tag:Fraser Complex; Gondwana break-up; central Westland; geochronology; lamprophyre
Volume:56
Issue:4
Number of pages:14
First page:229
Last Page:242
Funding institution:FRST [UOX1004]; Danish Research Council for Nature and Universe; QHAVDM [10-085245]
Organizational units:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Biochemie und Biologie
Peer review:Referiert
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