The flow of turbidity currents and pyroclastic flows into regions with topography produces
spatial variation in flow. This variation (the flow nonuniformity) affects not only the loci of …

This study reviews the thickness statistics of non-channelized turbidites from four tertiary
basins of Central-Northern Apennines (Italy), where bed geometry and sedimentary …

Confined turbidite basins are a common feature of many structurally complex continental
slopes, but their depositional history has never been characterized using outcrop data. A …

Stratigraphic trapping at pinch-out margins is a key feature of many turbidite-hosted
hydrocarbon reservoirs. In systems confined by lateral or oblique frontal slopes, outcrop …

This study investigates the depositional architecture of turbidite lobes from the Southern
Laga Basin (Lower Messinian, Central Apennines) and the external controls on its …

Tertiary foreland sedimentation in SE France occurred along the western sidewall of the
Alpine orogen during collision of the Apulian indentor with the European passive margin. A …

Turbidity currents distribute sediment across the seafloor, forming important archives of
tectonic and climatic change on the Earth's surface. Turbidity current deposition is affected …

A basin axial-channel belt was largely responsible for the observed distribution of coarse-
grained gravity-flow deposits in the Tertiary Puchkirchen and basal Hall formations of the …

Hybrid event beds are now recognized as an important component of many deep-sea fan
and sheet systems. They are interpreted to record the passage of rheologically complex …

ABSTRACT The European Alps are a mountain belt that is characterized by a series of
discrete orogenic events, which have long been recognized. Despite the inherent episodic …