Results 251 to 260 of about 117,153 (307)
Constraints of middle-late Permian granites in Eastern Inner Mongolia on the final subduction of the Paleo Asian Ocean. [PDF]
Zhao C, Yu Y, Liu Y, Cai H, He J, Gao X.
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Spatio-temporal constraints on thrusting across fold-and-thrust belts worldwide. [PDF]
Curzi M, Billi A, Carminati E, Tavani S.
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Sequence stratigraphy of the syn-rift miocene succession in the Abu Rudeis-Sidri Field, Gulf of Suez, Egypt. [PDF]
Assal EM +4 more
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Active Tectonics of Central Asia
Geotectonics, 2021Central Asia exceeds neighboring territories in the intensity of Quaternary uplifts and active faulting. The active fault kinematics differ in the northeast of the region, from Middle Tibet to Eastern Sayan, and its southern and western parts, including the Himalayas, the Pamir–Punjab syntaxis, and the region north of Gorny and Mongolian Altai.
V. G. Trifonov +3 more
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Russian Geology and Geophysics, 1995
Structural-geological and seismoacoustic studies carried out in 1989–94 within the Baikal Rift Zone show for the first time the internal active tectonic structure of the present Baikal Rift lake basin. A series of small structural features are distinguished not only by morphology but also by the degree of recent activity.
K. G. Levi +10 more
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Structural-geological and seismoacoustic studies carried out in 1989–94 within the Baikal Rift Zone show for the first time the internal active tectonic structure of the present Baikal Rift lake basin. A series of small structural features are distinguished not only by morphology but also by the degree of recent activity.
K. G. Levi +10 more
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Journal of Geophysical Research: Solid Earth, 1978
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.
Peter Molnar, Paul Tapponnier
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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.
Peter Molnar, Paul Tapponnier
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Quaternary tectonic activity in Scotland
Geological Society, London, Engineering Geology Special Publications, 1991Abstract The main features of seven faults inferred to have been active during the Quaternary in Scotland are summarized and their significance in terms of possible tectonic explanations is discussed. One fault in Glen Roy (Central Highlands) is described in detail and evidence is presented for changing stress fields inferred from modes of ...
Ringrose, PS +3 more
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Tectonophysics, 1992
Nearly 90 mm a−1 of relative plate convergence is absorbed in the Andean plate-boundary zone. The pattern of active tectonics shows remarkable variations in the way in which the plate slip vector is partitioned into displacement and strain and the ways in which compatibility between different segments is solved.
J.F. Dewey, S.H. Lamb
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Nearly 90 mm a−1 of relative plate convergence is absorbed in the Andean plate-boundary zone. The pattern of active tectonics shows remarkable variations in the way in which the plate slip vector is partitioned into displacement and strain and the ways in which compatibility between different segments is solved.
J.F. Dewey, S.H. Lamb
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Tectonically Active Landscapes
Environmental and Engineering Geoscience, 2011OK, I admit that I am a hard-rock geologist by training, and that I do not have formal education in geomorphology. However, my career has led me into seismic hazards assessment, where I have gained appreciation and respect for geomorphic methods used in assessing the age of fault movements (this from a person who once considered everything younger than
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