New study of continentalmargins could provide better understanding on the way to a carbon-neutral economy
. Top: zoom at the rift centre. Bottom: more general view of model. Red shade is plastic strain rate and blue is ductile strain rate. Grey shading shows accumulated plastic strain and represents areas where faulting occurred. Sediments are colour-coded by age since the start of rifting: in rainbow colours are sediments deposited during rifting and in white to red those deposited after breakup. Blue line marks the 10Pa s iso-viscosity line. Thin dotted black lines are isotherms.
Commonly interpreted to indicate seafloor spreading . Formed when mafic magma cools below the Curie point and takes the polarity of the Earth’s field at that time. data. Data that mainly records the near-normal incidence reflected waves and gives a high-resolution image of the reflectivity in the subsurface.Where the crust thins from the continental platform towards the distal domain . Necking zones can be spatially abrupt or occur over a large distance.
A reduction in the strength of the lithosphere due to mechanical damage. Strain weakening can result from the presence of fluids at faults, mineralization, reduction in grain size and the formation of crystallographic preferred orientations.Sediment deposited during the activity of the underlying basement faults.Boundaries between sedimentary rocks caused by a period of erosion or a pause in sediment accumulation. data.
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