It is well established that sedimentary margins grow by sediments bypassing through shelf-
and slope-incising canyons onto the basin floor and by sediments being deposited …

Process-product studies have been central to the development of process sedimentology
over the past few decades, with the ability to first measure flows, and then examine the …

Submarine sediment density flows are one of the most important processes for moving
sediment across our planet, yet they are extremely difficult to monitor directly. The speed of …

Turbidity currents, and other types of submarine sediment density flow, redistribute more
sediment across the surface of the Earth than any other sediment flow process, yet their …

Submarine gravity flows are a key process for transporting large volumes of sediment from
the continents to the deep sea. The location, volume, and character of the sediment …

Channel-levee systems are frequently interpreted as having a long history of cut-and-fill by
channel-shaped features of different scales. Results from a simple geometric model based …

Submarine channel-related thin-bedded turbidites are deposited in environments such as
external levees, internal levees, depositional terraces and at times of channel abandonment …

以松辽盆地齐家—古龙地区白垩系嫩江组一段为研究对象, 通过地震沉积学,
沉积构造和沉积序列等分析, 发现异重流成因的大型水道—湖底扇系统, 对大型坳陷湖盆深水区 …

The Cretaceous Tres Pasos Formation of southern Chile records a slope system
characterized by> 800 m of paleo-bathymetric relief. Channel deposits are exposed in an …

A never solved problem in sedimentary petrology is the origin of sandstone consisting
exclusively of quartz and most durable heavy minerals. The Congo River offers an excellent …