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In Situ Gas Content Prediction of Deep Coal Seams Based on Logging in the Central Linxing-Shenfu Block. [PDF]
Che Y +6 more
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Updated seismotectonic framework of Abu Dabbab Egypt based on focal mechanisms and stress inversion. [PDF]
Abdelazim M +7 more
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The Moral Consequences of the Arendtian Space of Freedom
Constellations, EarlyView.
Seung‐Hwan Hong
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Tectonic Stress Reconstruction Based on Structural Features in Tectonic Superposition Areas
Mining, Metallurgy and Exploration, 2020Tectonic stress is an important parameter for understanding the dynamics of underground engineering and for the exploitation of coalbed methane. Multiple-period structural features usually have complex spatial relationships in tectonic superposition areas, which provides evidence for identification of the sequence of the tectonic stress period ...
exaly +2 more sources
Stress variability and brittle tectonic structures
The problem of stress variability, both in space and time, during brittle deformation of rocks is faced in this note. Several possible causes of the temporal and spatial variations of the stress tensor are reviewed and discussed. A genetic partitioning of the stress tensor is proposed, showing that any stress field within a crustal volume can be seen ...
CAPUTO, Riccardo
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Tectonic stresses in the lithosphere
Tectonics, 1983Various types of observables (earthquake focal mechanisms, in situ measurements and geological deformations) give information about the large scale lithospheric stress field. The latter has often been explained by postulating appropriate forces acting at the edges and beneath the plates. This approach ignores the role of mass heterogeneities within the
Luce Fleitout, Claude Froidevaux
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Reviews of Geophysics, 1979
The state of stress in the lithosphere provides strong constraints on the forces acting on the plates. The directions of principal stresses in the plates as indicated by midplate earthquake mechanisms, in situ stress measurements, and stress‐sensitive geological features are used to test plate tectonic driving force models, under the premises that ...
Randall M. Richardson +2 more
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The state of stress in the lithosphere provides strong constraints on the forces acting on the plates. The directions of principal stresses in the plates as indicated by midplate earthquake mechanisms, in situ stress measurements, and stress‐sensitive geological features are used to test plate tectonic driving force models, under the premises that ...
Randall M. Richardson +2 more
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Apparent stress and stress drop for intraplate earthquakes and tectonic stress in the plates
pure and applied geophysics, 1977The magnitude of shear stress in the lithosphere is bounded from below by the apparent stress and stress drop during intraplate earthquakes. Apparent stresses and stress drops for a number of mid-plate earthquakes are calculated from the earthquake magnitude, SH wave amplitude spectra, and estimates of the length of the fault zone.
Randall M. Richardson, Sean C. Solomon
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1980
A flat jack method has been used to determine the principal stress axes in the Jurassic limestone of the basin of Paris and in neighbouring regions. The results have been compared with a few overcoring measurements in boreholes of a few meters.
C. Paquin, C. Froidevaux
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A flat jack method has been used to determine the principal stress axes in the Jurassic limestone of the basin of Paris and in neighbouring regions. The results have been compared with a few overcoring measurements in boreholes of a few meters.
C. Paquin, C. Froidevaux
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The origin of tectonic stress in the lithosphere
Tectonophysics, 1984Abstract The sources of lithospheric stress and their distinctive features are briefly reviewed. It is suggested that there are two main categories of lithospheric stress: renewable stress which persists despite continuing stress relaxation and non-renewable stress which can be dissipated by relief of the initial strain.
M.H.P. Bott, N.J. Kusznir
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