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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

Plate-moving mechanisms: their relative importance

TL;DR: In this article, the relative importance of different processes contributing to the motion of lithospheric plates probably varies during the assembly and break-up of Pangaea-type megacontinents.
Journal ArticleDOI

Mapping the mechanical anisotropy of the lithosphere using a 2D wavelet coherence, and its application to Australia

TL;DR: In this paper, a method for imaging the spatial variations of the anisotropy of the flexural response of the lithosphere, and apply it to recent topographic and gravity data sets over Australia.
Journal ArticleDOI

Left-lateral transtension along the Tierra Colorada deformation zone, northern margin of the Xolapa magmatic arc of southern Mexico

TL;DR: In this paper, structural analysis of steeply NNW-dipping tectonites along the northern margin of the Xolapa magmatic arc, southern Mexico, reveals progressive deformation involving ductile and brittle deformation mechanisms.
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Crustal ductile flow and its contribution to tectonic stress in Southwest China

TL;DR: In this article, the authors focus on the highland regions in Southwest (SW) China, including southeast Tibet and Sichuan and Yunnan provinces, to better understand the correlation between crustal stress and structural heterogeneities.
Journal ArticleDOI

Use of borehole imaging to improve understanding of the in-situ stress orientation of Central and Northern England and its implications for unconventional hydrocarbon resources

TL;DR: In this paper, the in-situ stress orientation of the Bowland-Hodder shales under Central and Northern England has been analyzed using high-resolution borehole imaging.
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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