Convolute bedding:Formation of convolute lamination in turbidites
Formation of convolute lamination in turbidites
由CGladstone著作·2018·被引用31次—Convolutelaminationisacommonfoldstructurewithinturbiditebeds,attributedtothedeformationofsedimentduringorsoonafterdepositionofthehost ...。其他文章還包含有:「a.Convolutebeddinginfine」、「Convolutebedding」、「ConvoluteLaminationinNon」、「Convolutelamination,itsorigin」、「Postdepositionalmodificationofsedimentarylayers」、「SedimentaryStructures」、「Soft」
查看更多 離開網站a. Convolute bedding in fine
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Each fining-up cycle is defined by a coarse-grained pebbly trough cross-stratified sandstone near the base and fine-grained, heterolithic sandstone-mudstone or ...
Convolute bedding
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Parallel lamination is widespread, and convolute bedding is usually present. These internal structures are arranged within wacke beds in a regular sequence.
Convolute Lamination in Non
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Convolute lamination and other sedimentary structures have been observed repeatedly in sequences characterized also by graded bedding.
Convolute lamination, its origin
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Convolute bedding occurs in both marine and nonmarine sediments of many environmental types. Although essentially syndepositional, its ...
Post depositional modification of sedimentary layers
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Convolute bedding and convolute lamination. The layering within sediments can be disrupted during or after deposition by localised and small ...
Sedimentary Structures
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It is loosely referred to as convolute bedding. On a smaller scale, laminated fine sands and silts also show penecontemporaneous vertical deformation ...
Soft
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Convolute bedding forms when complex folding and crumpling of beds or laminations occur. This type of deformation is found in fine or silty sands, and is ...