GRAVITY SURVEY OF LOWER AWATERE DISTRICT MARLBOROUGH, NEW ZEALAND

被引:8
作者
HUNT, TM
机构
[1] Geophysics Division, Department of Scientific and Industrial Research, Wellington
关键词
D O I
10.1080/00288306.1969.10431102
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Bouguer and residual gravity anomaly maps of the Lower Awatere District are presented. The gravity measurements support the concept that dip-slip faulting during the upper Tertiary was followed by transcurrent faulting in the Quaternary. A structural contour map of the top of the Torlesse Group basement derived from the residual gravity anomalies shows that the upper Tertiary rocks in the Lower Awatere Valley lie in a shallow basin centred about 3 miles east of Seddon. Positive residual anomalies over Torlesse Group greywackes are interpreted as resulting from basic igneous intrusions at depths less than 2 miles. © Taylor & Francis Group, LLC.
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页码:633 / &
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