Abstract In eastern Canada, the Charlevoix-Kamouraska/Bas-Saint-Laurent (CKBSL)
seismic zone presents a seismic hazard almost as high as that of the active Pacific zone …

Upper‐flow‐regime bedforms, including upper‐stage‐plane beds, antidunes, chutes‐and‐
pools and cyclic steps, are ubiquitous in glacigenic depositional environments characterized …

The monitoring of turbidity currents enables accurate internal structure and timing of these
flows to be understood. Without monitoring, triggers of turbidity currents often remain …

Glacier and ice sheet mass loss as a result of climate change is driving important coastal
changes in Arctic fjords. Yet limited information exists for Arctic coasts regarding the …

Abstract Systems Supplying Sediment to Canyon or Slope Channel Heads (SSSCHs)
initiate sediment transfer from the shallow water areas to the deep sea. SSSCHs are very …

In the eastern part of the Karoo Basin of South Africa, the sedimentary record of the Late
Palaeozoic Ice Age, the Dwyka Group, consists of an up to 200 m thick accumulation of …

Deglacial sedimentary sequences recording the decay and final demise of ice sheets result
from intricate interactions between the pattern of ice margin retreat, inherited basin …

与海相盆地重力流沉积研究理论的快速发展相比, 陆相湖盆重力流沉积的相关认识还存在着一定
差距. 综合国内, 外重力流沉积相关研究成果, 总结湖盆重力流沉积的相关认识 …

Cyclic‐step bedforms typifying a Froude‐supercritical flow regime are a recurrent
component of depositional/erosional turbiditic systems. Over modern delta slopes, cyclic …

The paleogeographic reconstruction of the successive inland positions of a retreating ice
sheet is generally constrained by mapping moraines. However, deltaic complexes …