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Statistical Methods in Sedimentary Petrology.1 Part I. Percentage Composition of Assemblages and their Graphical Study
Published online by Cambridge University Press: 01 May 2009
Extract
In recent years much work has been done in determining the quantitative—or more strictly “numerical”—composition of heavy mineral residues from sedimentary rocks in the hope of obtaining evidence as to whence the detritus was derived. It is clear that the petrological characteristics of the land mass whose erosion provides the detritus must always be an important factor in predetermining the percentage composition of the residue as we now find it. Yet the sorting action of the transporting agents (which tend to separate the heavy from the less heavy minerals) and of chemical agents (which, both before and after deposition, destroy some minerals and introduce new ones) may often be suspected of having a great or even a dominating influence upon the final composition of the residue. It is proposed in this paper to investigate by simple mathematical methods the probable effect of these processes and to do so along lines which have been suggested by the study of actual heavy mineral assemblages.
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- Copyright © Cambridge University Press 1939
Footnotes
These papers describe some statistical work chiefly on Jurassic and Triassic sediments in Yorkshire. The writer believes that the methods employed may be useful to other workers in attacking problems of sedimentary petrology, whilst the results lead to generalizations which may be worth testing elsewhere. Part II will deal with grain-size measurements and their graphical study, and Part III with the cartographic representation of numerical data.
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