JC Faugères, DAV Stow, P Imbert, A Viana - Marine Geology, 1999 - Elsevier
The sedimentary construction of oceanic margins is most often carried out by the combined action of gravitational processes and processes related to bottom (contour) currents. One of …
Nonrenewable energy resources, comprising fossil fuels and uranium, are not ran domly distributed within the Earth's crust. They formed in response to a complex array of geologic …
Deep-water sediment waves can be classified using a combination of grain size and wave- forming process, although in some cases one or other of these criteria may be …
KA Giles, MG Rowan - Geological Society, London, Special …, 2012 - lyellcollection.org
Halokinetic sequences are unconformity-bound packages of thinned and folded strata adjacent to passive diapirs. Hook halokinetic sequences have narrow zones of deformation …
WE Galloway - AAPG bulletin, 1998 - pubs.geoscienceworld.org
Subaqueous slope and base-of-slope depositional systems are a major component of most marine and many lacustrine basin fills, and constitute primary targets for hydrocarbon …
An overview of the main items concerning deep bottom-current-controlled deposits is presented. These include: the definition of contourites, their processes of deposition and …
ZR Jobe, DR Lowe, SJ Uchytil - Marine and Petroleum Geology, 2011 - Elsevier
Most submarine canyons are erosive conduits cut deeply into the world's continental shelves through which sediment is transported from areas of high coastal sediment supply onto large …
M Rebesco, D Stow - Marine Geophysical Researches, 2001 - Springer
Contourites are widespread throughout the deep sea, ranging from those that build up individually distinct bodies (mounded drifts) to those that occur closely interbedded with …
Publisher Summary Large-scale sediment waves are some of the most distinctive and frequently described depositional features generated by bottom currents, and cover huge …