Loch Burn Formation, Fiordland, New Zealand: SHRIMP U‐Pb ages, geochemistry and provenance
نویسندگان
چکیده
منابع مشابه
Patterns of Late Cenozoic exhumation deduced from apatite and zircon U-He ages from Fiordland, New Zealand
[1] New apatite and zircon (U-Th)/He ages from the Fiordland region of New Zealand’s South Island expand on earlier results and provide new constraints on patterns of Late Cenozoic exhumation and cooling across this region. Zircon (U-Th)/He cooling ages, in combination with increased density of apatite ages, show that in addition to a gradual northward decrease in cooling ages that was seen dur...
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متن کاملForest Understorey Changes after Reduction in Deer Numbers, Northern Fiordland, New Zealand
High deer numbers in northern Fiordland in the 1960s significantly changed forest understorey composition. The density of woody plants in the understorey was reduced in some areas by as much as 50%, and preferred plants became less abundant than those seldom eaten. However, the impact of deer and wapiti varied between forest types. Seral communities and silver beech forests at low altitudes in ...
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ژورنال
عنوان ژورنال: New Zealand Journal of Geology and Geophysics
سال: 2007
ISSN: 0028-8306,1175-8791
DOI: 10.1080/00288300709509829