This is the view to the west along the Gulf of Corinth active rift showing the bathymetry of the seafloor within the active offshore rift and a cross section beneath the seafloor interpreted from a seismic reflection profile. Red dashed lines on the seafloor and on the coast to the south are the major normal faults which control the region's morphology and the opening of the rift. Colored layers within the cross section represent layers of sediment deposited and deformed as the rift subsides. (Credit: NOCS)

ScienceDaily (Dec. 23, 2009) — A study of the structure and evolution of the Gulf of Corinth rift in central Greece will increase scientific understanding of rifted margin development and the tectonic mechanisms underlying seafloor spreading and deformation of the Earth's crust.

"The Gulf of Corinth rift is an ideal natural laboratory for studying early rift history," said Dr Lisa McNeill of the University of Southampton's School of Ocean and Earth Science (SOES) at the National Oceanography Centre, Southampton (NOCS): "The rift is less than five million years old and is relatively easy to interpret as its structure has not been significantly complicated by geological events over a long period of time. The rifting process is also the source of hazardous earthquakes in the region."

Using available marine and terrestrial data, including high-resolution seismic reflection profiles from a research cruise aboard the MV Vasilios in 2003, the researchers analysed fault evolution across the entire rift system, producing a fault framework for the rift and revealing patterns of basin subsidence through rift history. They also estimated when faults became active and the rates at which they slip.

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