作者: D. Calvin Campbell , David C. Mosher
DOI: 10.1016/J.MARGEO.2015.10.005
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摘要: Abstract Two-dimensional and three-dimensional multichannel seismic reflection data are utilized to examine previously unrecognized contourite depositional systems along the continental margin of Nova Scotia, Canada. Prior this study these features were thought be limited extent in area. The new show that drifts widespread with greatest drift development during Late Miocene Pliocene. Giant sediment waves form stacked, aggrading sequences bedforms their is linked pre-existing seafloor morphology. Small developed locally throughout late Paleogene Neogene, either southwest down-current obstacles or channel fills. Major erosional pulses regional markers; first rise Early Oligocene, then slope Three-dimensional erosion surfaces preserve along-slope amplitude anomalies, two-dimensional, low-relief waves, barchanoid bedforms. geophysical evidence implies a northeast-to-southwest, bottom current influenced Cenozoic patterns