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An evaluation of geochemical weathering indices in loess-paleosol studies

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TLDR
In this paper, the Chemical Proxy of Alteration (CPA) is proposed as the most appropriate index for silicate weathering, which is based on the molar ratio Al 2O3/(Al2O3+Na2O)×100.
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This article is published in Quaternary International.The article was published on 2011-08-01. It has received 366 citations till now. The article focuses on the topics: Weathering.

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Quantifying chemical weathering intensity and trace element release from two contrasting basalt profiles, Deccan Traps, India

TL;DR: In this paper, the mafic index of alteration (MIA) was proposed to quantify the net loss of the mobile major elements (Ca, Mg, Na, K +/- Fe) relative to the immobile major elements(Al +/- Fe).
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Provenance control on chemical indices of weathering (Taiwan river sands)

TL;DR: In this article, the concentration of chemical elements in terrigenous sediments is constrained by the original mineralogy of source rocks, and is thus provenance-dependent, and the mineralogy and geochemistry of sediments may undergo substantial modifications by diverse physical processes during transport and deposition, including recycling and hydraulic sorting by size, density or shape, and/or by chemical dissolution and precipitation during diagenesis.
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Provenance versus weathering control on the composition of tropical river mud (southern Africa)

TL;DR: In this paper, the authors present an integrated mineralogical-geochemical database on fine-grained sediments transported by all major rivers of southern Africa, including the Zambezi, Okavango, Limpopo, Olifants, Orange and Kunene.
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Pleistocene environmental dynamics recorded in the loess of the middle and lower Danube basin

TL;DR: The Danubian loess stratigraphy comprises distinct loess-paleosol sequences, reflecting glacial-interglacial phases which can be quantified for intensity using environmental magnetism and geochemistry as mentioned in this paper.
References
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The continental crust: Its composition and evolution

TL;DR: In this paper, the authors describe the composition of the present upper crust and deal with possible compositions for the total crust and the inferred composition of lower crust, and the question of the uniformity of crustal composition throughout geological time is discussed.
Book

Trace elements in soils and plants

TL;DR: The Biosphere The Anthroposphere Soils and Soil Processes Weathering Processes Pedogenic Processes Soil Constituents Trace Elements Minerals Organic Matter Organisms in Soils Trace Elements in Plants.
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Environmental Chemistry of Soils

M. B. McBride
TL;DR: In this article, an introduction to modern soil chemistry describes chemical processes in soils in terms of established principles of inorganic, organic, and physical chemistry, providing an understanding of the structure of the solid mineral and organic materials from which soils are formed.
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Early Proterozoic climates and plate motions inferred from major element chemistry of lutites

TL;DR: The early Proterozoic Huronian Supergroup of the north shore of Lake Huron (Fig. 1) is a thick succession of sedimentary and volcanic rocks deposited between about 2,500 and 2,100 Myr ago as discussed by the authors.

World Reference Base for Soil Resources 2006

TL;DR: The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries.
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