Journal Article10.1016/S0037-0738(87)80006-4
Inclined heterolithic stratification—Terminology, description, interpretation and significance
Richard G. Thomas,Derald G. Smith,James M. Wood,John Visser,E. Anne Calverley-Range,Emlyn H. Koster +5 more
633
TL;DR: Inclined Heterolithic Stratification (IHS) as discussed by the authors is a nomenclature for inclined stratified sedimentary units. But it is not suitable for the case of point bars.
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About: This article is published in Sedimentary Geology. The article was published on 01 Jun 1987. The article focuses on the topics: Cross-bedding.
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The sedimentology of the Middle and Upper Border groups (Viséan) in the Stonehaugh Borehole, Northumberland
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Superimposed allogenic and biological controls on siliciclastic architecture: an early mississippian (visean) example from tropical laurussia
William J. McMahon,Harm Jan Pierik,Anthony P. Shillito,F. Salese,Bart Van Der Kwaak,Daniel R. Parsons,Maarten G. Kleinhans +6 more
TL;DR: In this article , a sedimentological analysis is given for the Mississippian (Visean) siliciclastic strata which crop out in counties Donegal and Mayo in NW Ireland.
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References
Architectural-Element Analysis: A New Method of Facies Analysis Applied to Fluvial Deposits
TL;DR: In this article, the authors proposed a new method of analysis for fluvial facies, which subdivides fluvic deposits into local suites consisting of one or more of a set of eight basic three-dimensional architectural elements.
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A review of the origin and characteristics of recent alluvial sediments
TL;DR: In this paper, the geometrical, textural, structural, and biological characteristics of alluvial sediments are reviewed with respect to their geometrically, texturally, structural and biological properties, which are related to the physiographic occurrence and hydraulic geometry of streams and to the dynamics of flowing water.
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•Book
Sedimentology of Gravels and Conglomerates
Emlyn H. Koster,Ronald J. Steel +1 more
- 01 Jun 1984
TL;DR: In this article, a review of diagnostic features and facies sequences of alluvial/marine systems is presented, and particular effort must be made to extract maximum information from the individual bed characteristics.
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