The geological and geodynamic condition on the formation of the Dabashan thrust nappe structure, Based on FLAC numerical modelling
La estructura de la falla de cabalgamiento de las montaąs Dabashan en el margen sur del cinturn̤ orogňico de Qinling sufri ̤por lo menos dos etapas de evolucin̤, la colisin̤ orogňica del Tris̀ico Superior entre el bloque de la China del Norte, la microplaca de Qinling y el bloque Yangtze, y la or...
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| Online dostop: | The geological and geodynamic condition on the formation of the Dabashan thrust nappe structure, Based on FLAC numerical modelling |
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