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In geology, transpression is a type of str … In geology, transpression is a type of strike-slip deformation that deviates from simple shear because of a simultaneous component of shortening perpendicular to the fault plane. This movement ends up resulting in oblique shear. It is generally very unlikely that a deforming body will experience "pure" shortening or "pure" strike-slip. The relative amounts of shortening and strike-slip can be expressed in the convergence angle alpha which ranges from zero (ideal strike-slip) to 90 degrees (ideal convergence). During shortening, unless material is lost, transpression produces vertical thickening in the crust. Transpression that occurs on a regional scale along plate boundaries is characterized by oblique convergence. More locally, transpression occurs within restraining bends in strike-slip fault zones.training bends in strike-slip fault zones.
, 走滑挤壓（英語：Transpression）是一種走滑變形之一，它與簡單的剪切變形不同之處，在於同時具有垂直於斷層走向的挤壓分量。這種運動最終會導致斜剪切。構造變形通常不太可能是“純” 挤壓或“純”走滑變形。挤壓和走滑的相對量可以用收斂角 α 表示，範圍從零（純走滑）到 90 度（純挤壓）。遭擠壓的地殼會在地殼中產生垂直增厚。走滑挤壓在板塊邊界中由斜向聚合造成。 在局部地區，走滑挤壓是在走滑斷裂帶的約约束弯曲内造成。
, La transpressione in geologia è un tipo di … La transpressione in geologia è un tipo di deformazione da scorrimento che si discosta da un semplice taglio a causa di una componente simultanea di compressione perpendicolare al piano di faglia. Questo movimento causa alla fine un taglio obliquo. In generale è molto improbabile che un corpo che si deforma subisca una compressione "pura" o uno "scorrimento orizzontale" puro. Le quantità relative di compressione e di scivolamento possono essere espresse dall'angolo di convergenza alfa che va da zero (scorrimento orizzontale ideale) a 90 gradi (convergenza ideale). Durante la compressione, a meno che non si perda materiale, la transpressione produce un ispessimento verticale nella crosta. La transpressione che si verifica su scala regionale lungo i bordi delle placche è caratterizzata dalla convergenza obliqua. Più localmente, la transpressione si verifica all'interno di piegature di contenimento in zone di faglie a scorrimento orizzontale. zone di faglie a scorrimento orizzontale.
, Транспрессия — , сочетающий условия сдвига … Транспрессия — , сочетающий условия сдвига и сжатия. Зоны транспрессии образуются в случае, если сдвиговая зона испытывает дополнительное боковое сжатие. Показателями зон транспрессии являются взбросо-сдвиги и так называемые структуры цветка (структуры пальмового дерева), представляющие собой пакеты тектонических пластин выдавленных из зоны сдвига.ческих пластин выдавленных из зоны сдвига.
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Транспрессия — , сочетающий условия сдвига … Транспрессия — , сочетающий условия сдвига и сжатия. Зоны транспрессии образуются в случае, если сдвиговая зона испытывает дополнительное боковое сжатие. Показателями зон транспрессии являются взбросо-сдвиги и так называемые структуры цветка (структуры пальмового дерева), представляющие собой пакеты тектонических пластин выдавленных из зоны сдвига.ческих пластин выдавленных из зоны сдвига.
, In geology, transpression is a type of str … In geology, transpression is a type of strike-slip deformation that deviates from simple shear because of a simultaneous component of shortening perpendicular to the fault plane. This movement ends up resulting in oblique shear. It is generally very unlikely that a deforming body will experience "pure" shortening or "pure" strike-slip. The relative amounts of shortening and strike-slip can be expressed in the convergence angle alpha which ranges from zero (ideal strike-slip) to 90 degrees (ideal convergence). During shortening, unless material is lost, transpression produces vertical thickening in the crust. Transpression that occurs on a regional scale along plate boundaries is characterized by oblique convergence. More locally, transpression occurs within restraining bends in strike-sliprs within restraining bends in strike-slip
, La transpressione in geologia è un tipo di … La transpressione in geologia è un tipo di deformazione da scorrimento che si discosta da un semplice taglio a causa di una componente simultanea di compressione perpendicolare al piano di faglia. Questo movimento causa alla fine un taglio obliquo. In generale è molto improbabile che un corpo che si deforma subisca una compressione "pura" o uno "scorrimento orizzontale" puro. Le quantità relative di compressione e di scivolamento possono essere espresse dall'angolo di convergenza alfa che va da zero (scorrimento orizzontale ideale) a 90 gradi (convergenza ideale).e ideale) a 90 gradi (convergenza ideale).
, 走滑挤壓（英語：Transpression）是一種走滑變形之一，它與簡單的剪切變形不同之處，在於同時具有垂直於斷層走向的挤壓分量。這種運動最終會導致斜剪切。構造變形通常不太可能是“純” 挤壓或“純”走滑變形。挤壓和走滑的相對量可以用收斂角 α 表示，範圍從零（純走滑）到 90 度（純挤壓）。遭擠壓的地殼會在地殼中產生垂直增厚。走滑挤壓在板塊邊界中由斜向聚合造成。 在局部地區，走滑挤壓是在走滑斷裂帶的約约束弯曲内造成。
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| rdfs:label |
Transpressione
, Транспрессия
, 走滑挤壓
, Transpression
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