Depositional patterns within syn-tectonic stratal units give insights into the spatial characteristics of the fault zone at particular stages of its evolution.
The correlation is supported by an analysis of stratal expansion, throw development, and data on the sandstone ratio of corresponding footwall and hanging-wall intervals.
These stratal patterns have recently been described in detail and their significance fully discussed by Braga et al…
This stratal geometry is common in temperate carbonates.
This study demonstrates a close relationship between sedimentary styles and stratal geometries resulting from progradation of specific sedimentary systems.
This study exemplifies very clearly the sort of stratal geometries that result from the progradation of specific, temperate carbonate sedimentary systems.
Similar stratal geometries have been described from comparable levels in the Chalk of the North Sea, and in outcrop in Britain and France.
If these progradational features are indicative of true stratal geometries they suggest significant transport of sediment across the sea bed during deposition.
However, although many of the reflection terminations appear indicative of stratal truncation it may not be the only cause of reflection termination.
The basic characteristics of a stratal unit may be strongly controlled by source-area lithology.
The stratal geometries that are characteristic of the unconformity depend strongly on structural and geographical position within the basin.
Below the downward tapering cone, stratal geometries change to a dominantly convex-up form defining a minor, upwards pointing cone that is reminiscent of reactive diapir geometry.
Strong, continuous stratal reflections characterize the shallow subsurface on the upper and middle shelf.
Rhymes
startle
Definition of stratal in US English:
stratal
adjectiveˈstrādl
Relating or belonging to strata or a stratum.
层的，有关层的
Example sentencesExamples
Similar stratal geometries have been described from comparable levels in the Chalk of the North Sea, and in outcrop in Britain and France.
However, although many of the reflection terminations appear indicative of stratal truncation it may not be the only cause of reflection termination.
If these progradational features are indicative of true stratal geometries they suggest significant transport of sediment across the sea bed during deposition.
The correlation is supported by an analysis of stratal expansion, throw development, and data on the sandstone ratio of corresponding footwall and hanging-wall intervals.
Below the downward tapering cone, stratal geometries change to a dominantly convex-up form defining a minor, upwards pointing cone that is reminiscent of reactive diapir geometry.
The stratal geometries that are characteristic of the unconformity depend strongly on structural and geographical position within the basin.
This study demonstrates a close relationship between sedimentary styles and stratal geometries resulting from progradation of specific sedimentary systems.
The basic characteristics of a stratal unit may be strongly controlled by source-area lithology.
This study exemplifies very clearly the sort of stratal geometries that result from the progradation of specific, temperate carbonate sedimentary systems.
This stratal geometry is common in temperate carbonates.
These stratal patterns have recently been described in detail and their significance fully discussed by Braga et al…
Depositional patterns within syn-tectonic stratal units give insights into the spatial characteristics of the fault zone at particular stages of its evolution.
Strong, continuous stratal reflections characterize the shallow subsurface on the upper and middle shelf.