Aegean tectonics: Strain localisation, slab tearing and trench retreat
We review the geodynamic evolution of the Aegean–Anatolia region and discuss strain
localisation there over geological times. From Late Eocene to Present, crustal deformation in …
localisation there over geological times. From Late Eocene to Present, crustal deformation in …
Rifted margin architecture and crustal rheology: reviewing Iberia-Newfoundland, central South Atlantic, and South China Sea
Crustal rheology controls the style of rifting and ultimately the architecture of rifted margins.
Here we review the formation of three magma-poor margin pairs, Iberia-Newfoundland, the …
Here we review the formation of three magma-poor margin pairs, Iberia-Newfoundland, the …
Strain migration during multiphase extension: Observations from the northern North Sea
Many rifts develop through multiphase extension; it can be difficult, however, to determine
how strain is distributed during reactivation because structural and stratigraphic evidence …
how strain is distributed during reactivation because structural and stratigraphic evidence …
Rapid spatiotemporal variations in rift structure during development of the Corinth Rift, central Greece
Abstract The Corinth Rift, central Greece, enables analysis of early rift development as it is
young (< 5 Ma) and highly active and its full history is recorded at high resolution by …
young (< 5 Ma) and highly active and its full history is recorded at high resolution by …
Tectono‐sedimentary evolution of the Plio‐Pleistocene Corinth rift, Greece
The onshore central Corinth rift contains a syn‐rift succession> 3 km thick deposited in 5–15
km‐wide tilt blocks, all now inactive, uplifted and deeply incised. This part of the rift records …
km‐wide tilt blocks, all now inactive, uplifted and deeply incised. This part of the rift records …
Fault architecture, basin structure and evolution of the Gulf of Corinth Rift, central Greece
The style of extension and strain distribution during the early stages of intra‐continental
rifting is important for understanding rift‐margin development and can provide constraints for …
rifting is important for understanding rift‐margin development and can provide constraints for …
Tectono‐sedimentary evolution of the western Corinth rift (Central Greece)
M Ford, S Rohais, EA Williams, S Bourlange… - Basin …, 2013 - earthdoc.org
Abstract The Corinth rift (Greece) is one of the world's most active rifts. The early Plio‐
Pleistocene rift is preserved in the northern Peloponnese peninsula, south of the active …
Pleistocene rift is preserved in the northern Peloponnese peninsula, south of the active …
The structures, stratigraphy and evolution of the Gulf of Corinth rift, Greece
B Taylor, JR Weiss, AM Goodliffe… - Geophysical Journal …, 2011 - academic.oup.com
A multichannel seismic and bathymetry survey of the central and eastern Gulf of Corinth
(GoC), Greece, reveals the offshore fault geometry, seismic stratigraphy and basin evolution …
(GoC), Greece, reveals the offshore fault geometry, seismic stratigraphy and basin evolution …
Fault displacement rates on a range of timescales
Displacements on tectonic faults primarily accrue during earthquakes at rates that vary
through time. To examine the processes that underlie the temporal changes in fault …
through time. To examine the processes that underlie the temporal changes in fault …
Comparison of methods to estimate sediment flux in ancient sediment routing systems
CJ Brewer, GJ Hampson, AC Whittaker… - Earth-Science …, 2020 - Elsevier
The need to predict accurately the volume, timing and location of sediments that are
transported from an erosional source region into a basin-depocentre sink is important for …
transported from an erosional source region into a basin-depocentre sink is important for …