The stratified shungite-bearing deposits that retain sedimentary structures are interpreted as vesicles and forming the matrix to breccias, are interpreted as migrated petroleum, now in the form of metamorphosed bitumen.
42.
"' Interference Ripples "'are a type of sedimentary structure made up of two sets of ripples formed at right-angles to each other as a result of there being two dominant paleocurrents.
43.
Depositional environments in ancient sediments are recognised using a combination of sedimentary facies, facies associations, sedimentary structures and fossils, particularly trace fossil assemblages, as they indicate the environment in which they lived.
44.
His reconstructions of Wealden palaeography and depositional environments have been based on meticulous examination and analysis of faecies changes, sedimentary structures and petrology combined with a study of modern deltaic and littoral sedimentation.
45.
Critical examinations of these reported fossils have concluded that the fossil sponges are inorganic silica concretions; the jellyfish are either gas escape structures or algal colonies; and the worm trails are inorganic sedimentary structures.
46.
In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e . g ., tabular and trough cross-bedding and graded bedding.
47.
The location from which the specimen was derived, the Gaulin Dinosaur Tracksite, has been interpreted as a playa, or dry lake environment based on the presence of oscillation ripple marks, abundant mudcracks, and other sedimentary structures.
48.
At least three distinct facies types have been identified and distinguished on the basis of sedimentary structures and grain size : a hummocky cross stratified facies, a trough-cross stratified facies, and a large scale-cross stratified facies.
49.
It has initiated " �volution du littoral danubien : vuln�rabilit?et pr�vention " project which is to collect seismic data from the mouth of the river Danube, to study the morpho-sedimentary structure of the river-sea system.
50.
In large enough and hot enough magma chambers, where vigorous convection currents form, pseudo-sedimentary structures such as flow banding, graded bedding, scour channels, foreset beds and other usually sedimentary features can be created by convection and settling processes.
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