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The space between framework components either is empty or is filled with chemical cement, finer-than-granule clasts, or both.
Three major framework components can be identified within this deposit: (a) sheet-like sandstone aprons, (b) channel-fill sandbodies and (c) lensoid massive beds of pebbly sandstone.
The latest trends as well as both theoretical and technological research advances pose challenges used in the representation of information used by the framework components of this domain.
Particular attentions are devoted to inelastic modelling of framework components for accurate representation of frame behaviour and the applications of plastic hinge analysis for large-scale framework.
A set of statistical experiments is used to benchmark the framework components and shows that this approach requires no extensive training for generalisation and can adapt to environmental changes flexibly.
An overview of quantitative approaches to analysis and modelling of sediment generation and provenance is presented, with an emphasis on major framework components as determined by means of petrographic techniques.
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Wackes (the second triangular panel of Figure 4) consist of a sand-size framework component floating in a finer-grained pasty matrix of grains finer than 0.03 millimetre whose overall abundance exceeds 15 percent by volume.
Arenites (the front triangular panel of Figure 4) consist of a sand-size framework component surrounded by pore spaces that are either empty (in the case of arenite sands) or filled with crystalline chemical cement (in the case of arenites).
Fatigue and fast fracture tests were performed to determine the Weibull distribution of lifetime and initial mechanical strength for each framework component.
Quartz is the predominant framework component in the sandstones, usually constituting 45% 55% % of the whole rock volume with an average framework composition of Q51F28R21.
Each framework component is discussed in detail below.
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