Journal Article10.1029/JB083IB11P05361
Active tectonics of Tibet
Peter Molnar,Paul Tapponnier +1 more
764
TL;DR: In this paper, an interpretation of Landsat imagery of Tibet shows that the most recent structures appear to be normal faults that trend approximately north-south, and the fault plane solutions of 14 earthquakes in the central part of the Tibetan plateau indicate large components of normal faulting.
read more
Abstract: From an interpretation of Landsat imagery of Tibet the most recent structures appear to be normal faults that trend approximately north-south. Fault plane solutions of 14 earthquakes in the central part of the Tibetan plateau indicate large components of normal faulting. The solutions are not well constrained, but for the most reliable ones the T axes are oriented approximately east-west. Only on the margins of the high plateau, where elevations are lower, do fault plane solutions show active thrust faulting. These observations imply an east-west extension of most of Tibet at the present time. We relate this pattern to the collision of India and Eurasia and to deformation of an especially weak Tibetan crust and upper mantle. India applies a pressure to Eurasia that maintains Tibet at a high uniform altitude, and the hydrostatic head caused by this elevation transmits the pressure northward. Accordingly, Tibet is the pressure gauge of Asia. At the same time a small east-west strain (or flow) of the lower crust and upper mantle of Tibet would stretch the surface layer. Tibet's position relative to India at the present time is analogous to that of a ‘dead’ triangle in a plastic material indented by a rigid indenter (India).
read more
Chat with Paper
AI Agents for this Paper
Find similar papers on Google Scholar, PubMed and Arxiv
Write a critical review of this paper
Analyze citations of this paper to find unaddressed research gaps
Citations
Earthquake source characteristics along the arcuate Himalayan belt: Geodynamic implications
TL;DR: In this article, a positive correlation between plate and stress obliquities is established for this diffuse plate boundary, and the authors propose that the zone of sharp bending of the descending Indian lithosphere is the nodal area of major stress accumulation which is released occasionally in form of earthquakes.
Crustal structure of western Tibet revealed by Lg attenuation tomography
TL;DR: The lateral Lg wave attenuation in western Tibet and surrounding regions is studied in this paper, where the Lg phases are extracted from the vertical component of seismograms with magnitude greater than 4.6 mb and focal depth less than 50 km to measure the TSM and RTSM Lg Q at 1 Hz (Q0).
15
Surge-tectonic evolution of southeastern Asia: a geohydrodynamics approach
TL;DR: In this article, the authors show that mantle diapirs as proposed by traditional plate-tectonic models do not exist; there is no discernible pattern of upper or lower mantle convection, and thus no longer an adequate mechanism to move plates; and the lithosphere above a depth of about 80 km is permeated by an interconnected network of low-velocity channels.
14
Discourse on Seismotectonics of Nepal Himalaya and Vicinity:Appraisal to Earthquake Hazard
Daya Shanker,Harihar Paudyal,Harminder Singh +2 more
- 31 Aug 2012
TL;DR: In this paper, the authors have shown that the central part of the Himalayas is one of the most seismically active regions in the Himalayan arc and that the thrusting decreases rapidly with increasing focal depth and deformation occurs due to strike-slip motion at greater depths.
Structural characteristics of middle and southern Xainza-Dinggye Normal Fault System and its relationship to South-ern Tibetan Detachment System
TL;DR: The Southern Tibetan Detachment System (STDS) is expressed as a ductile shear zone composed of mylonitic leucogranite in the studied area of this note as mentioned in this paper.
14
References
•Book
The mathematical theory of plasticity
Rodney Hill
- 01 Jan 1950
TL;DR: In this paper, the solution of two-dimensional non-steady motion problems in two dimensions is studied. But the solution is not a solution to the problem in three dimensions.
8.3K
Cenozoic Tectonics of Asia: Effects of a Continental Collision: Features of recent continental tectonics in Asia can be interpreted as results of the India-Eurasia collision.
Peter Molnar,Paul Tapponnier +1 more
TL;DR: The JSTOR Archive is a trusted digital repository providing for long-term preservation and access to leading academic journals and scholarly literature from around the world, supported by libraries, scholarly societies, publishers, and foundations.
4.3K
Tibetan, Variscan, and Precambrian Basement Reactivation: Products of Continental Collision
John F. Dewey,Kevin Burke +1 more
TL;DR: In this article, the authors consider that continental collision is followed by crustal thickening, to accommodate further plate convergence, with ensuing partial melting of the lower crust, resulting in a dry refractory lower crust consisting of pyroxene granulites and anor-thosites.
925
Slip-line field theory and large-scale continental tectonics
Paul Tapponnier,Peter Molnar +1 more
TL;DR: In this paper, a simple analogy is made between the tectonics of Asia and deformation in a rigidly indented rigid-plastic solid, where India is analogous to the indenter and the great strike-slip faults correspond to slip lines.
818