New Zealand Journal of Geology and Geophysics abstracts
Gravity anomalies and crustal loading at and adjacent to the Alpine Fault, New
Zealand
T. A. STERN
Research School of Earth Sciences
Victoria University of Wellington
P.O. Box 600
Wellington, New Zealand
Abstract An analysis of Bouguer and isostatic gravity
anomalies from the convergent plate boundary, central South Island, New
Zealand, is developed using constraints from seismic refraction data, plate
tectonics, and an elastic flexure model. Between 50 and 80 km of late Tertiary
plate convergence is assumed so that relatively dense, subducted mantle is
included in the gravity model. An elastic plate with a free edge and an
effective elastic thickness (
Te) that varies laterally between 10 and 30
km is used to simulate the deflection of the Pacific plate beneath the central
South Island. Loading on the plate is in the form of topography of the Southern
Alps and the excess mass of subducted Pacific mantle. For a weak plate with
Te = 10 km, only 50 km of subducted plate, and hence convergence, is
required to explain the Bouguer gravity anomalies. For a stronger plate model,
where
Te varies between 15 and 35 km, c. 80 km of convergence is
required. The latter model is preferred as it is more consistent with a seismic
determination for dip on top of the Pacific plate. Neither model gives an ideal
fit to the observed Bouguer gravity anomalies, thus underscoring the
limitations and assumptions inherent in a two-dimensional elastic plate
analysis. The most important departure from a simple elastic plate model occurs
over the eastern South Island, where a zone of 30 mgal isostatic gravity
anomalies exist. These gravity highs are, instead, accounted for by crustal
loading of mobile greywacke-schist rocks that have been thrust upwards and
sideways by the pressure of the growing orogen in the central South Island.
Keywords gravity anomalies; subduction load; flexure; crustal
root; crustal loading; paleobathymetry
New Zealand Journal of Geology and Geophysics, 1995, Vol. 38: 593-600
0028-8306/95/3804-0593 $2.50/0 (c) The Royal Society of New Zealand
1995
PDF file of entire paper: medium quality (835K); (scanned from paper original: notes about this process)
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