Fault geometry and evidence of depocentre migration within a transtensional intra-basinal high – a case study from the Łączna Anticline (Intrasudetic Synclinorium, SW Poland) | Zendy

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Fault geometry and evidence of depocentre migration within a transtensional intra-basinal high – a case study from the Łączna Anticline (Intrasudetic Synclinorium, SW Poland)

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