turbidite

He has written over 100 scientific papers and several books on stratigraphy and turbidite systems.

Provenance work on the turbidite sandstones has indicated at least two sources for heavy minerals.

Sole markings are found most commonly in turbidite deposits.

This has allowed facies and structural modelling of the turbidite systems in the Llanilar district.

They may, in fact, explain many of the curious features of so-called "turbidite" and similar sequences.

In the Carboniferous it starts with a turbidite sequence containing basic volcanics.

These are interpreted as a turbidite sequence.

The top layer consists of turbidite sequence from the Early Ordovician.

It is a small turbidite oil and gas field produced under natural depletion using subsea manifolds.

Biological material found in the turbidite enabled it to be dated to between 381 and 612, consistent with the date of the Tauredunum event.

Modified drift-turbidite systems refer to the interactions of contourite and turbidite deposits.

This lateral migration only style of sinuosity is believed to be somewhat rare in occurrence within turbidite systems.

They are the only common macrofossils in the basinal turbidite terrain that underlies the greater part of these regions.

The majority of the zone is covered by Late Visean turbidite sequences several kilometres thick.

These include debris flows and turbidite flows.

Above the turbidite facies are shallow marine mudstones and then deltaic sandstones.

Turbidite deposits typically occur in foreland basins.

A turbidite bed has been recognised in the Çınarcık Basin, whose deposition matches the date of the earthquake.

In the southern part of the range the bedrock is overlaid by Eocene age turbidite sediments and river sediment.

The suspended load is carried out the furthest into the body of water than all other types of sediment creating a turbidite.

Landslides from the caldera rim thereafter formed debris fans and turbidite sediments on the lake bed.

The group is subdivided into formations, which each represent a turbidite lobe, and are separated by anoxic background sedimentation.

In: Examples of turbidite facies and associations from selected formations of the northern Apennines.

Graptolites in the thick turbidite sequences of central Wales are often finely preserved as three dimensional moulds, sometimes even with the original periderm.

Fleming - this field has a Palaeocene Maureen Formation turbidite sandstone reservoir pinching out to the east.