. "Thin-skinned deformation is a style of deformation in plate tectonics at a convergent boundary which occurs with shallow thrust faults that only involves cover rocks (typically sedimentary rocks), and not deeper basement rocks. In the rock record, this will increase the influence of more surficial rocks, which usually includes sedimentary rocks. Typically, repeated sections of the same rock are seen over and over as thrust faults, coming up from the decollement, stack the same layer on top of itself. The sediments that are created by this type of deformation are typically lithic sandstones."@en . . . "25702663"^^ . . "La tect\u00F2nica de pell fina \u00E9s un dels estils de deformaci\u00F3 tect\u00F2nica que pot tenir lloc en situacions d'escur\u00E7ament de l'escor\u00E7a continental, caracteritzat per l'apilament d'encavalcaments que afecten principalment a la coberta sediment\u00E0ria i en menor mesura al basament cristal\u00B7l\u00ED. El terme es contraposa al de tect\u00F2nica de pell gruixuda, estil de deformaci\u00F3 que presenta fractures d'escala cortical. L'estil de deformaci\u00F3 de pell fina \u00E9s t\u00EDpic dels cinturons de plecs i mantells de corriment que voregen alguns or\u00F2gens, particularment quan existeixen bons nivells d'enlairament, com a capes de lutites o evaporites"@ca . "La tect\u00F2nica de pell fina \u00E9s un dels estils de deformaci\u00F3 tect\u00F2nica que pot tenir lloc en situacions d'escur\u00E7ament de l'escor\u00E7a continental, caracteritzat per l'apilament d'encavalcaments que afecten principalment a la coberta sediment\u00E0ria i en menor mesura al basament cristal\u00B7l\u00ED. El terme es contraposa al de tect\u00F2nica de pell gruixuda, estil de deformaci\u00F3 que presenta fractures d'escala cortical."@ca . "La tect\u00F3nica de piel fina es uno de los estilos de deformaci\u00F3n tect\u00F3nica que puede ocurrir en situaciones de acortamiento de la corteza continental, caracterizado por el apilamiento de cabalgamientos que afectan principalmente a la cobertera sedimentaria y en menor medida al basamento cristalino.\u200B El t\u00E9rmino se contrapone al de tect\u00F3nica de piel gruesa, estilo de deformaci\u00F3n que presenta fracturas de escala cortical. El estilo de deformaci\u00F3n de piel fina es t\u00EDpico de los cinturones de pliegues y mantos de corrimiento que bordean algunos or\u00F3genos, particularmente cuando existen buenos niveles de despegue, tales como capas de lutitas o evaporitas\u200B"@es . "1058575348"^^ . . . "La tect\u00F3nica de piel fina es uno de los estilos de deformaci\u00F3n tect\u00F3nica que puede ocurrir en situaciones de acortamiento de la corteza continental, caracterizado por el apilamiento de cabalgamientos que afectan principalmente a la cobertera sedimentaria y en menor medida al basamento cristalino.\u200B El t\u00E9rmino se contrapone al de tect\u00F3nica de piel gruesa, estilo de deformaci\u00F3n que presenta fracturas de escala cortical."@es . "\u8584\u76AE\u8B8A\u5F62"@zh . . "\u8584\u76AE\u8B8A\u5F62\uFF08\u82F1\u8A9E\uFF1Athin-skinned deformation\uFF09\u662F\u677F\u584A\u69CB\u9020\u5728\u805A\u5408\u6027\u677F\u584A\u908A\u7DE3\u7684\u4E00\u7A2E\u8B8A\u5F62\uFF0C\u5B83\u767C\u751F\u5728\u6DFA\u9006\u885D\u65B7\u5C64\u4E2D\uFF0C\u50C5\u6D89\u53CA\u8986\u84CB\u5CA9\uFF08\u901A\u5E38\u662F\u6C89\u7A4D\u5CA9\uFF09\uFF0C\u800C\u4E0D\u6D89\u53CA\u66F4\u6DF1\u7684\u57FA\u5E95\u5CA9 \u3002\u8584\u76AE\u8B8A\u5F62\u901A\u5E38\u5F62\u6210\u5728\u78B0\u649E\u5E36\u524D\u9678\u6216\u706B\u5C71\u5F27\u5F8C\u5F27\u7B49\u8655\u767C\u80B2\u7684\u8936\u76BA\u548C\u9006\u885D\u5E36\u4E2D\u3002\u82E5\u5E95\u90E8\u6709\u6ED1\u8131\u9762\u5B58\u5728\uFF0C\u5982\u9801\u5CA9\u3001\u84B8\u767C\u5CA9\u6216\u9AD8\u5B54\u9699\u6D41\u9AD4\u58D3\u529B\u3002\u8584\u76AE\u8B8A\u5F62\u66F4\u7232\u986F\u8457\u3002\u5176\u69CB\u9020\u5730\u5C64\u4E5F\u5305\u542B\u591A\u6B21\u91CD\u8907\u5730\u5C64\u7232\u7279\u5FB5 \u3002"@zh . . "Thin-skinned estilo tektonikoa edo azaleko estilo tektonikoa plaka tektonikoen arteko muga konbergenteetan aurkitzen diren lurraldeetan gara daitekeen eskala handiko deformazio-eredua da. Estilo tektonikoaren ezaugarri nagusia zamalkaduren nagusitasuna da, deformazio gehiena xurgatzen dute eta deformazio-estiloa kontrolatzen dute. Deformazioa lurrazaleko lehendabiziko kilometroetan ematen da, eta oinaldeko-zamalkadura nagusitik (sole fault) behera ez da deformaziorik gertatzen. Estilo tektonikoa bereziki orogenoetako toles eta zamalkadura gerrikoetan ematen da."@eu . . "Thin-skinned estilo tektonikoa edo azaleko estilo tektonikoa plaka tektonikoen arteko muga konbergenteetan aurkitzen diren lurraldeetan gara daitekeen eskala handiko deformazio-eredua da. Estilo tektonikoaren ezaugarri nagusia zamalkaduren nagusitasuna da, deformazio gehiena xurgatzen dute eta deformazio-estiloa kontrolatzen dute. Deformazioa lurrazaleko lehendabiziko kilometroetan ematen da, eta oinaldeko-zamalkadura nagusitik (sole fault) behera ez da deformaziorik gertatzen. Estilo tektonikoa bereziki orogenoetako toles eta zamalkadura gerrikoetan ematen da."@eu . . . . . . . . . . . "Thin-skinned deformation"@en . . "Azaleko estilo tektoniko"@eu . . "Tect\u00F3nica de piel fina"@es . "2596"^^ . . . . . . . . . . "Tect\u00F2nica de pell fina"@ca . . . . . "\u8584\u76AE\u8B8A\u5F62\uFF08\u82F1\u8A9E\uFF1Athin-skinned deformation\uFF09\u662F\u677F\u584A\u69CB\u9020\u5728\u805A\u5408\u6027\u677F\u584A\u908A\u7DE3\u7684\u4E00\u7A2E\u8B8A\u5F62\uFF0C\u5B83\u767C\u751F\u5728\u6DFA\u9006\u885D\u65B7\u5C64\u4E2D\uFF0C\u50C5\u6D89\u53CA\u8986\u84CB\u5CA9\uFF08\u901A\u5E38\u662F\u6C89\u7A4D\u5CA9\uFF09\uFF0C\u800C\u4E0D\u6D89\u53CA\u66F4\u6DF1\u7684\u57FA\u5E95\u5CA9 \u3002\u8584\u76AE\u8B8A\u5F62\u901A\u5E38\u5F62\u6210\u5728\u78B0\u649E\u5E36\u524D\u9678\u6216\u706B\u5C71\u5F27\u5F8C\u5F27\u7B49\u8655\u767C\u80B2\u7684\u8936\u76BA\u548C\u9006\u885D\u5E36\u4E2D\u3002\u82E5\u5E95\u90E8\u6709\u6ED1\u8131\u9762\u5B58\u5728\uFF0C\u5982\u9801\u5CA9\u3001\u84B8\u767C\u5CA9\u6216\u9AD8\u5B54\u9699\u6D41\u9AD4\u58D3\u529B\u3002\u8584\u76AE\u8B8A\u5F62\u66F4\u7232\u986F\u8457\u3002\u5176\u69CB\u9020\u5730\u5C64\u4E5F\u5305\u542B\u591A\u6B21\u91CD\u8907\u5730\u5C64\u7232\u7279\u5FB5 \u3002"@zh . "Thin-skinned deformation is a style of deformation in plate tectonics at a convergent boundary which occurs with shallow thrust faults that only involves cover rocks (typically sedimentary rocks), and not deeper basement rocks. The thin-skinned style of deformation is typical of many fold and thrust belts developed in the foreland of a collisional zone or back arc of a continental volcanic arc. This is particularly the case where a good basal decollement exists, usually in a weaker layer like a shale, evaporite, or a zone of high pore fluid pressure. This was first described in Rocky Mountains of the United States, as part of the Sevier Orogeny. In the rock record, this will increase the influence of more surficial rocks, which usually includes sedimentary rocks. Typically, repeated sections of the same rock are seen over and over as thrust faults, coming up from the decollement, stack the same layer on top of itself. The sediments that are created by this type of deformation are typically lithic sandstones."@en .