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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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Journal ArticleDOI

The forces driving the plates : constraints from kinematics and stress observations. Discussion

TL;DR: In this paper, a torque balance model is used to describe the evolution of plate dynamics over the Cenozoic Era for reconstructions of plate geometry and velocities, and stress models which incorporate the forces are compared with stress orientations for the North and South American plates.
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CASMI-A visualization tool for the World Stress Map database

TL;DR: Two stress map examples generated with CASMI ranging from plate-wide to regional scale are presented: A stress map of central Europe, that reveals the correlation of stress field orientation and relative plate motion, and the fan-shape stress pattern in North Germany.
Journal ArticleDOI

Stress fields acting during lithosphere breakup above a melting mantle: A case example in West Greenland

TL;DR: In this paper, the authors characterize and map the stress fields acting during plate breakup along the West Greenland volcanic margin, based on an inversion of fault-slip data sets and magma-driven fractures, crosscutting mainly an exposed inner seaward-dipping basaltic wedge (SDRi: inner Seaward Dipping Reflectors).
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New seismic images of the Central Indian Suture Zone and their tectonic implications

TL;DR: In this article, the authors used the common reflection surface (CRS) stack method to image the Central Indian Suture (CIS), a mega shear zone located in the central part of the Indian shield.
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The build-up and triggers of volcanic eruptions

TL;DR: In this paper, the authors discuss the processes leading up to volcanic eruptions, by following the journey of magma from crustal storage zones to the surface, and discuss the accumulation and evolution of volcanic storage regions, the processes that trigger magma reservoir failure and the ascent of the magma through the crust.
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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