strike-slip fault
falla de desenganche · falla de desgarre · falla de desplazamiento horizontal · falla transcurrente
strike slip fault oor Spaans
strike slip fault
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falla de desenganche
falla de desgarre
The Dead Sea Fault (DSF) is an important strike-slip fault that cuts across several countries in the eastern Mediterranean.
La Falla del Mar Muerto es una importante falla de desgarre que atraviesa varios países de la región oriental del Mediterráneo.
falla de desplazamiento horizontal
falla transcurrente
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All are right lateral-moving strike-slip faults.
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Identification of the main fault trends (‘strike-slip faults’);
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There are no strike-slip faults, no volcanic activity.
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The north-south Kazerun strike-slip fault divides the Zagros into two distinct zones of deformation.
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The main NNE-SSW trending fault systems show a mixture of dextral (right lateral) strike-slip faulting and reverse faulting.
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Mafic rocks are associated with strike-slip faults and normal faults and are found in the southern Puna and Altiplano.
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The Dead Sea Fault (DSF) is an important strike-slip fault that cuts across several countries in the eastern Mediterranean.
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The North Anatolian Fault and the Northeast Anatolian Fault, which are east–west-running strike-slip faults, run along the length of the range.
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The northern portion of the Trench is dominated by strike-slip faulting, while the southern part of the Trench was created by normal faults.
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The ridge's movement may also have changed the type of faulting along the coast, causing strike-slip faults (faults that move horizontally past each other).
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The existence of important strike-slip faults running highly oblique to the main regional structural pattern and controlling the shape of the Sierras Subandinas folds has been verified.
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The provinces are further divided into terranes – large slices of crust with different geological histories that have been brought together by tectonic activity (subduction and strike-slip faulting) to form New Zealand.
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According to the US Geological Survey, the earthquake was caused by sections of the earth rubbing alongside each other at vertical, or nearly vertical, fracture points in what is known as a strike-slip fault.
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The Garlock Fault is a left-lateral strike-slip fault running northeast-southwest along the north margins of the Mojave Desert of Southern California, for much of its length along the southern base of the Tehachapi Mountains.
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The clearest evidence is located at the Potreros zone, where strike-slip faults with orientation N60°W and NNE affect the present course of the Herradura River, in addition to tilting and differential uplifting when compared with the adjacent terraces.
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At 01:25 JST on April 16 (16:25 UTC, April 15), a 7.0 magnitude earthquake, under Higashi Ward of Kumamoto City in the Kyushu Region in southwest Japan, occurred as the result of strike-slip faulting at shallow depth.
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The convergence between these plates is highly oblique near Sumatra, with the displacement being accommodated by near pure dip-slip faulting along the subduction zone, known as the Sunda megathrust, and near pure strike-slip faulting along the Great Sumatran fault.
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Focal mechanisms solution from P and pP polarities shows a strike slip faulting, where one of the nodal planes has strike 272o (east-west orientation), dip 86o and slip angle -172o, and the other one has strike 181o (north-south orientation), dip 82o and slip angle -4o.
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In the context of plate tectonics, strike-slip movement of the Tintina Fault on the Tintina-Northern Rocky Mountain Trench is also related to strike-slip movement along the San Andreas Fault, the extension of the Basin and Range Province, and other extensional or strike-slip fault systems in western North America.
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The aforementioned basement ramp along which orogeny-related thrust faulting and subsequent strike-slip and normal faulting occurred is probably associated with the ancient continental shelf of Paleozoic and Mesozoic time.
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While the principal faults in the region are of the strike-slip type, a significant thrust fault (with no surface trace) is found on the mountain's southwest flank.
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Right-lateral strike-slip movement of the Tintina Fault on the Tintina-Northern Rocky Mountain Trench may have begun during the middle Jurassic.
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These highly oblique faults with strike-slip movements, that affect the whole region, are probably ancient lineaments reactivated during Andean diastrophism in Upper Pliocene to Early Pleistocene time.
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The varying geometry of these folds is interpreted partly as being due to the existence of previous en échelon folds related to the strike-slip component of the faults and, partly, as a result of the variable intensity of the shear strain undergone during the first variscan phase.
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121 sinne gevind in 12 ms. Hulle kom uit baie bronne en word nie nagegaan nie.