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Active Deformation of Asia: From Kinematics to Dynamics

England, Philip, Molnar, Peter·1997·Science

Abstract

Using estimated strain rates across the actively deforming region of Asia to infer variations in viscous stress, it is shown that gradients of stress point uphill toward the center of Tibet, where gravitational potential energy per unit surface area reaches a maximum. Thus, the dynamics of the deformation seem to obey the equation of creeping flow, which expresses a balance between gradients in stress and the gravitational body force. This balance, in the region of the Tibetan plateau, yields an estimate of 10 22 pascal second for the average viscosity of the Tibetan lithosphere, which is only about 10 to 100 times greater than the viscosity of the convecting upper mantle.

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Metadata

Authors
England, P., & Molnar, P.
Venue
Science
Published
1997-10-24
Volume
278
Issue
5338
Pages
647-650
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2067135199
Cited by
506
References
0
FWCI
8.77
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Active Deformation of Asia: From Kinematics to Dynamics. https://app.cochat.ai/papers/10.1126/science.278.5338.647
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England, P., & Molnar, P. (1997). Active Deformation of Asia: From Kinematics to Dynamics. Science. https://doi.org/10.1126/science.278.5338.647

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.