Print Email Facebook Twitter The structure of the Lavagna Nappe in the region of Monte Ramaceto and Val Graveglia (Ligurian Apennines, Italy) Title The structure of the Lavagna Nappe in the region of Monte Ramaceto and Val Graveglia (Ligurian Apennines, Italy) Author van Zutphen, A.C.A. van Wamel, W.A. Brons, A.J. Project Molengraaff Fonds Date 1984 Abstract Detailed structural analysis and mapping in the Lavagna Nappe reveals the effect of various phases of deformation on a regional scale. The earliest phase produced large isoclinal, originally SW-facing folds (F1). A second phase led to the development of open folds (F2). The vergence of the younger folds (F3, F4) is NE. Thrusting occurred in two stages: postF2-pr F3 and synF4. Hereafter the previously stacked thrustsheets, together forming the Lavagna Nappe, were emplaced on top of the Melange Nappe by NE-directed trusting. A final phase of gentle folding (F5) caused an undulation of all older structures. To reference this document use: http://resolver.tudelft.nl/uuid:d3d454e5-fac7-4798-a2e6-17e75fdaa21d Publisher Utrecht University Part of collection Geoscience Reports Document type report Rights (c) the author(s) Files PDF Zuthpen-Wamel-Bons (1984).pdf 6.65 MB Close viewer /islandora/object/uuid:d3d454e5-fac7-4798-a2e6-17e75fdaa21d/datastream/OBJ/view