The processes of underthrusting and underplating in the geologic record: Structural diversity between the Franciscan Complex (California), the Kodiak Complex …
F Meneghini, M Marroni, JC Moore… - Geological …, 2009 - Wiley Online Library
Existing studies on active subduction margins have documented the wide diversity in
structural style between accretionary prisms, both in space and time. Together with physical
boundary conditions of the margins, the thickness of sedimentary successions carried by the
lower plate seems to play a key role in controlling the deformation and fluid flow during
accretion. We have tested the influence of the subducting sedimentary section by comparing
the structural style and fluid‐related structures of four units from three fossil accretionary …
structural style between accretionary prisms, both in space and time. Together with physical
boundary conditions of the margins, the thickness of sedimentary successions carried by the
lower plate seems to play a key role in controlling the deformation and fluid flow during
accretion. We have tested the influence of the subducting sedimentary section by comparing
the structural style and fluid‐related structures of four units from three fossil accretionary …
The processes of underthrusting and underplating in the geologic record: structural diversity between the Franciscan Complex (California), the Kodiak Complex …
F Meneghini - RENDICONTI DELLA SOCIETÀ GEOLOGICA …, 2012 - arpi.unipi.it
Existing studies on active subduction margins have documented the wide diversity in
structural style between accretionary prisms, both in space and time. Together with physical
boundary conditions of the margins, the thickness of sedimentary successions carried by the
lower plate seems to play a key role in controlling the deformation and fluid flow during
accretion. We have tested the influence of the subducting sedimentary section by comparing
the structural style and fluid-related structures of four units from three fossil accretionary …
structural style between accretionary prisms, both in space and time. Together with physical
boundary conditions of the margins, the thickness of sedimentary successions carried by the
lower plate seems to play a key role in controlling the deformation and fluid flow during
accretion. We have tested the influence of the subducting sedimentary section by comparing
the structural style and fluid-related structures of four units from three fossil accretionary …
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