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Mid-ocean ridges (MORs) are quintessential sites of tectonic extension1,2,3,4, at which divergence between lithospheric plates shapes abyssal hills that cover about two-thirds of the Earth’s surface5,6. Here we show that tectonic extension at the ridge axis can be partially undone by tectoni...
Here, the 1-to-5 km-thick sedimentary succession comprises a basal pelagic layer overlainby sediments of the Nicobar submarine fan. Drill sites are located at 3°N 91°E, ~ 250 km southwest of thesubduction zone, on the eastern flank of the Ninetyeast Ridge where the input section is ~...
(675 km) east to west. They consist of a number of separate banks, chief of which are Grand, Green, and St. Pierre; and they are sometimes considered to include the submarineplateausthat extend southwestward toGeorges Bank, east-southeast ofCape Cod, Massachusetts, U.S. Depths average 180...