New Zealand Journal of Geology and Geophysics abstracts
An episodic Cretaceous cooling model for the Otago-Marlborough Schist,
New Zealand, based on 40Ar/39Ar white mica ages
TIMOTHY A. LITTLE
School of Earth Sciences
Victoria University of Wellington
P.O. Box 600
Wellington, New Zealand
email: timothy.little@vuw.ac.nz
NICK MORTIMER
Institute of Geological and Nuclear Sciences
Private Bag 1930
Dunedin, New Zealand
email: n.mortimer@gns.cri.nz
MICHAEL MCWILLIAMS
Geophysics Department
Stanford University
Stanford, CA 94305-2215
USA
email: mac@pangea.stanford.edu
Abstract New 40Ar/39Ar ages of 12 white
mica samples from deep levels of the Otago and Marlborough Schists, together
with previously published whole-rock K-Ar ages yield a nonlinear age-depth
profile suggesting a fossil partial retention zone for argon. In contrast to
earlier studies, we interpret (1) the peak of Otago Schist metamorphism to have
occurred in the Middle Jurassic (170-180 Ma) rather than Early Jurassic; and
(2) subsequent cooling to have been episodic, not slow and continuous. These
data cannot be modelled uniquely but support a model where the schist was held
at mid to lower crustal depths until c. 135 +/- 5 Ma, after which it was
rapidly unroofed at 0.6-1.0 mm/yr during regional crustal thickening along the
eastern margin of New Zealand. We infer that there were also one or more
younger periods of argon loss affecting deep levels of the Otago/Marlborough
Schists in a spatially heterogeneous way after c. 120 Ma. Late Cretaceous argon
loss at <75-84 Ma coincided with seafloor spreading offshore of New Zealand
and probably involved crustal reheating. Post-mid Cretaceous phases of argon
loss may have coincided with periods of heat input into the crust, including
metamorphism of the Alpine Schist at deep levels of the Haast Schist.
Keywords Cretaceous tectonics; Ar-Ar geochronology; Haast
Schist; Otago Schist; Marlborough Schist; cooling history
New Zealand Journal of Geology & Geophysics, 1999, Vol. 42:
305-325
0028-8306/99/4203-0305 $7.00/0 (c) The Royal Society of New Zealand
1999
PDF file of entire paper: medium quality (2206K); (scanned from paper original: notes about this process)
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