Magmatism during Gondwana breakup: new geochronological data from Westland, New Zealand

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

  • Quinten van der Meer
  • J.M. Scott
  • Waight, Tod
  • M. Sudo
  • A. Schersten
  • A.F. Cooper
  • T.L. Spell

Newly determined Late Cretaceous 40Ar/39Ar 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

OriginalsprogEngelsk
TidsskriftNew Zealand Journal of Geology and Geophysics
Vol/bind56
Udgave nummer4
Sider (fra-til)229-242
Antal sider14
ISSN0028-8306
DOI
StatusUdgivet - 2013

ID: 45455739