Results 211 to 220 of about 9,157 (264)
Geodetic Constraints on Segment-Scale Slip Rates and Interseismic Coupling Along the Havran-Balıkesir Fault Zone, NW Anatolia, Türkiye. [PDF]
Tiryakioğlu İ +12 more
europepmc +1 more source
Tectonic and climatic implications of the Aleutian Arc initiation ≥56 million years ago. [PDF]
Hoernle K +13 more
europepmc +1 more source
Study on the genesis mechanism of geothermal resources in the Yunkai area, South China based on geophysical data. [PDF]
Zhou Y +7 more
europepmc +1 more source
Beyond the Populist Moment: Nationalism and the Democratic Chain of Conflict
Constellations, EarlyView.
Michaelangelo Anastasiou
wiley +1 more source
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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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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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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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ACTIVE TECTONICS OF THE AEGEAN REGION
Annual Review of Earth and Planetary Sciences, 1994The Aegean Sea and its surrounding regions comprise one of the most rapidly deforming parts of the Alpine-Himalayan mountain belt. Though the deformation of the belt as a whole is related to thc northward move ment of Africa, Arabia, and India relative to Eurasia, the tectonics of the Aegean region itself is dominated by strike-slip and extensional ...
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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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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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