[HTML][HTML] A new classification system for mixed (turbidite-contourite) depositional systems: Examples, conceptual models and diagnostic criteria for modern and ancient …

S Rodrigues, FJ Hernández-Molina, M Fonnesu… - Earth-Science …, 2022 - Elsevier
Interactions between along-slope bottom currents and down-slope turbidity flows can create
a myriad of features and deposits. Despite numerous efforts to differentiate contourites from …

Challenging the highstand-dormant paradigm for land-detached submarine canyons

MS Heijnen, F Mienis, AR Gates, BJ Bett… - Nature …, 2022 - nature.com
Sediment, nutrients, organic carbon and pollutants are funnelled down submarine canyons
from continental shelves by sediment-laden flows called turbidity currents, which dominate …

The Quaternary sedimentary history and dynamics of the deep-water margin off the Hudson Strait ice stream

H Rashid, DJW Piper - Quaternary Science Reviews, 2024 - Elsevier
Sites of ice-stream discharge to the continental slope build trough-mouth fans from
glacigenic debris flows (GDFs), subglacial meltwater flows, and suspended sediment. Thus …

Influence of sedimentary processes and fault tectonics on the evolution of submarine canyons in the East Andaman Basin: Insights from high-resolution seismic data …

L Jin, X Luan, TD Raveendrasinghe, L Jiang, Y Xue… - Geomorphology, 2024 - Elsevier
Abstract The Andaman Sea Basin, a well-known back-arc spreading centre and a mature
petroliferous basin, presents a unique and complex scenario for understanding the interplay …

[HTML][HTML] Bottom current control on sediment deposition between the Iselin Bank and the Hillary Canyon (Antarctica) since the late Miocene: an integrated seismic …

R Conte, M Rebesco, L De Santis, F Colleoni… - Deep Sea Research …, 2021 - Elsevier
In this paper we analyze how oceanic circulation affects sediment deposition along a sector
of the Ross Sea continental margin, between the Iselin Bank and the Hillary Canyon, and …

Glaciomarine sediment deposition on the continental slope and rise of the central Ross Sea since the Last Glacial Maximum

S Ha, E Colizza, F Torricella, L Langone, F Giglio… - Marine Geology, 2022 - Elsevier
The continental margin of the Ross Sea has been consistently sensitive to the advance and
retreat of the Ross Ice Sheet (RIS) between the interglacial and glacial periods. This study …

Pleistocene depositional environments and links to cryosphere-ocean interactions on the eastern Ross Sea continental slope, Antarctica (IODP Hole U1525A)

MV King, JA Gales, JS Laberg, RM McKay, L De Santis… - Marine Geology, 2022 - Elsevier
The repeated proximity of West Antarctic Ice Sheet (WAIS) ice to the eastern Ross Sea
continental shelf break during past ice age cycles has been inferred to directly influence …

Pliocene–Pleistocene warm-water incursions and water mass changes on the Ross Sea continental shelf (Antarctica) based on foraminifera from IODP Expedition 374

JL Seidenstein, RM Leckie, R McKay… - Journal of …, 2024 - jm.copernicus.org
Abstract International Ocean Discovery Program (IODP) Expedition 374 sailed to the Ross
Sea in 2018 to reconstruct paleoenvironments, track the history of key water masses, and …

Environmental and oceanographic conditions at the continental margin of the Central Basin, northwestern Ross Sea (Antarctica) since the last glacial maximum

F Torricella, R Melis, E Malinverno, G Fontolan… - Geosciences, 2021 - mdpi.com
The continental margin is a key area for studying the sedimentary processes related to the
advance and retreat of the Ross Ice Shelf (Antarctica); nevertheless, much remains to be …

Tectonic and oceanographic controls on the slope-confined dendritic canyon system in the Dongsha Slope, South China Sea

X Wang, F Cai, Z Sun, Q Li, A Li, Y Sun, H Wang, Q Sun - Geomorphology, 2022 - Elsevier
Dendritic canyon system is the most widespread type of submarine canyons along
continental margins and plays important roles in sediment delivery and deep-water …