Lateral variability of the erosive plate boundary in the Northern Apennines, Italy
作者： Francesca Remitti , Giuseppe Bettelli , Paola Vannucchi
DOI: 10.3301/IJG.2012.11
关键词: Subduction 、 Tectonics 、 Slip (materials science) 、 Plate tectonics 、 Geomorphology 、 Laminar flow 、 Petrology 、 Geology
摘要: The early to middle Miocene erosive plate boundary preserved in the Northern Apennines NW of Sillaro Line is formed by two distinct units - Sestola-Vidiciatico Tectonic Unit and Subligurian Units. These occupy, respectively, SE portions studied area. Upon closer examination, features that distinguish these mapped do not reflect differing processes, but rather incorporation or non-incorporation forearc-toe mass-wasting deposits into active subduction channel. In other respects, document similar channel including contemporaneous activity multiple sub-parallel slip surfaces. This mode deformation leads ‘laminar' stacked slices within
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