Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/13675
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Type: Journal article
Title: The origins of the Australian stress field
Author: Coblentz, D.
Sandiford, M.
Richardson, R.
Zhou, S.
Hillis, R.
Citation: Earth and Planetary Science Letters, 1995; 133(3-4):299-309
Publisher: Elsevier
Issue Date: 1995
ISSN: 0012-821X
Statement of
Responsibility: 
David D. Coblentz, Mike Sandiford, Randall M. Richardson, Shaohua Zhou, Richard Hillis
Abstract: The ridge push force acting on the Indo-Australian plate exerts a significant torque (8.5 × 10²⁵N m) about a pole at 30.3°N, 34.5°E. The angular difference between this torque pole and the observed pole of rotation for the plate (19.2°N, 35.6°E) is less than 12° and suggests that the ridge push force plays an important role in the dynamics of the Indo-Australian plate. We have used an elastic finite-element analysis to study the predicted intraplate stress field in continental Australia for four models which employ different boundary conditions to balance the ridge push torque acting on the plate. The modeling indicates that a number of important features of the observed stress field within the Australian continent can be explained in terms of balancing the ridge push torque with resistance imposed along the Himalaya, Papua New Guinea, and New Zealand collisional boundaries segments. These features include N---S-to NE-SW-oriented compression in the northern Australia and E-W-oriented compression in southern Australia. Our analysis also shows that subduction processes along the northern and eastern boundaries provide only second-order controls on the intraplate stress field in continental Australia.
RMID: 0030003621
DOI: 10.1016/0012-821X(95)00084-P
Appears in Collections:Geology & Geophysics publications

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