Convolute bedding：Convolute lamination, its origin
Convolute lamination, its origin
由SDzuynski著作·1963·被引用113次—Convolutebeddingoccursinbothmarineandnonmarinesedimentsofmanyenvironmentaltypes.Althoughessentiallysyndepositional,its ...。其他文章還包含有：「a.Convolutebeddinginfine」、「Convolutebedding」、「ConvoluteLaminationinNon」、「Formationofconvolutelaminationinturbidites」、「Postdepositionalmodificationofsedimentarylayers」、「SedimentaryStructures」、「Soft」
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a. Convolute bedding in fine
https://www.researchgate.net
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
https://www.britannica.com
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
https://www.jstor.org
Convolute lamination and other sedimentary structures have been observed repeatedly in sequences characterized also by graded bedding.
Formation of convolute lamination in turbidites
https://strathprints.strath.ac
Convolute lamination is a common fold structure within turbidite beds, attributed to the deformation of sediment during or soon after deposition of the host ...
Post depositional modification of sedimentary layers
http://geologylearn.blogspot.c
Convolute bedding and convolute lamination. The layering within sediments can be disrupted during or after deposition by localised and small ...
Sedimentary Structures
https://epgp.inflibnet.ac.in
It is loosely referred to as convolute bedding. On a smaller scale, laminated fine sands and silts also show penecontemporaneous vertical deformation ...
Soft
https://en.wikipedia.org
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 ...