作者: Mirko Francioni , Paolo Pace , Milena Vitulli , Nicola Sciarra , Fernando Calamita
DOI: 10.1017/S0016756819000050
关键词: Culmination 、 Shear (geology) 、 Transverse plane 、 Foreland basin 、 Anticline 、 Seismology 、 Geology 、 Hinge line
摘要: The distribution of joints, veins and shear fractures in the Montagna dei Fiori overturned anticline is here reported. Two joint sets, longitudinal transverse to NNW–SSE axial trend, a conjugate system fractures, are recognized. sets have pre-folding development likely related foreland/foredeep flexure. joints were reopened during layer-parallel shortening along with fractures. Then, syn-folding outer-arc extension hinge-line culmination fold-axial parallel extension, both enhanced reactivated, respectively.