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Global patterns of tectonic stress

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TLDR
In this article, the authors used regional patterns of present-day tectonic stress to evaluate the forces acting on the lithosphere and to investigate intraplate seismicity, and found that most intraplate regions are characterized by a compressional stress regime; extension is limited almost entirely to thermally uplifted regions.
Abstract
Regional patterns of present-day tectonic stress can be used to evaluate the forces acting on the lithosphere and to investigate intraplate seismicity. Most intraplate regions are characterized by a compressional stress regime; extension is limited almost entirely to thermally uplifted regions. In several plates the maximum horizontal stress is subparallel to the direction of absolute plate motion, suggesting that the forces driving the plates also dominate the stress distribution in the plate interior.

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Citations
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Journal ArticleDOI

Asynchronizing paleo-Pacific slab rollback beneath SE China: Insights from the episodic Late Mesozoic volcanism

TL;DR: Zhang et al. as discussed by the authors proposed an asynchronizing paleo-Pacific slab rollback model to account for the episodic magmatism and crustal extension in SE China.
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Plate tectonics, plate moving mechanisms and rifting

TL;DR: In this paper, a sequence of palaeo-reconstructions of the distribution of continents in the Western Hemisphere suggests that frictional forces exerted on the base of the lithosphere by the slowly convecting sub-lithospheric upper mantle play an important role as a driving mechanism of plate movements.
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Role of tectonic stress in seepage evolution along the gas hydrate‐charged Vestnesa Ridge, Fram Strait

TL;DR: In this paper, the influence of tectonic stress on seepage evolution along the ~100 km long hydrate-bearing Vestnesa Ridge in Fram Strait was discussed.
Journal ArticleDOI

Reconciling Short Recurrence Intervals with Minor Deformation in the New Madrid Seismic Zone

TL;DR: P Paleoseismological data indicate that earthquakes large enough to cause soil liquefaction have occurred several times in the past 5000 years, but pervasive crustal deformation expected from such a high frequency of large earthquakes is not observed.
Journal ArticleDOI

Tectonic forces controlling the regional intraplate stress field in continental Australia: Results from new finite element modeling

TL;DR: In this paper, a finite element analysis of the intraplate stresses in the Indo-Australian plate (IAP) is provided by an observed regional stress field based on observations in 12 stress provinces, and a weighted basis set method is employed to evaluate a very large number of tectonic force combinations and to make a quantitative assessment of the fit between the observed and predicted stress fields.
References
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Journal ArticleDOI

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, +1 more
- 08 Aug 1975 - 
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.
Journal ArticleDOI

An analysis of the variation of ocean floor bathymetry and heat flow with age

TL;DR: In this paper, a simple cooling model and the plate model were proposed to account for the variation in depth and heat flow with increasing age of the ocean floor. But the results were limited to the North Pacific and North Atlantic basins.

Present-day plate motions

TL;DR: A data set comprising 110 spreading rates, 78 transform fault azimuths, and 142 earthquake slip vectors has been inverted to yield a new instantaneous plate motion model, designated Relative Motion 2 (RM2).
Journal ArticleDOI

Present‐day plate motions

TL;DR: In this article, a data set comprising 110 spreading rates, 78 transform fault azimuths and 142 earthquake slip vectors was inverted to yield a new instantaneous plate motion model, designated RM2.
Journal ArticleDOI

On the Relative Importance of the Driving Forces of Plate Motion

TL;DR: In this paper, the relative strength of the plausible driving forces, given the observed motions and geometries of the lithospheric plates, was analyzed. But the results indicate that the forces acting on the downgoing slab control the velocity of the oceanic plates and are an order of magnitude stronger than any other force.
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