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Book ChapterDOI

Green Clay Minerals

Bruce Velde
- 01 Jan 2014 - 
- Vol. 9, pp 351-364
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TLDR
In this article, a reference is made concerning color, to thin section microscopic perception, based largely upon old data, those which combine iron oxidation states and XRD information, which can reflect either compositional differences, mineral structure differences, or differences in geological occurrence.
Abstract
Color poses a problem for scientific study The first problem is the vocabulary one uses to describe color Mint green, bottle green, and kelly green are nice names but not of great utility in that people's physical perception of color is not always the same A second problem is that color in a spectral identification is the result of several absorption emissions, with overlapping signals, forming a complicated spectrum Interpretation depends greatly on the spectrum of the light source and the conditions of transmission–reflection of the sample In this chapter, reference is made concerning color, to thin section microscopic perception The discussion is based largely upon old data, those which combine iron oxidation states and XRD information It seems clear that green clay mineral names can reflect either compositional differences, mineral structure differences, or differences in geological occurrence

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Citations
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Journal ArticleDOI

The glauconite–Fe‐illite–Fe‐smectite problem: a critical review

TL;DR: In this paper, the compositional fields of glaucony, Fe-illite, and Fe-Al smectites are determined in the M+/4Si vs. Fe/Sum of octahedral cations (M+ ǫ=interlayer charge).
Journal ArticleDOI

Clay Mineralogy, Organic Carbon Burial, and Redox Evolution in Proterozoic Oceans

TL;DR: In this article, the authors analyzed the mineralogy, geochemistry and total organic carbon (TOC) of organic rich shales deposited in late Archean to early Cambrian sedimentary basins.
Journal ArticleDOI

Formation of syngenetic and early diagenetic iron minerals in the late Archean Mt. McRae Shale, Hamersley Basin, Australia: New insights on the patterns, controls and paleoenvironmental implications of authigenic mineral formation

TL;DR: A section of the late Archean Mt. McRae Shale comprising, in ascending order, a lower shale interval (LSI), a banded iron formation (BIF), an upper shale (USI) and a carbonate (C1) has been analyzed for total Fe and Al contents and authigenic Fe present as carbonate, oxide, sulfide and silicate phases.
Journal ArticleDOI

A Compositional Classification For Grain Assemblages In Fine-Grained Sediments and Sedimentary Rocks—Reply

TL;DR: A tripartite compositional classification is proposed for sediments and sedimentary rocks that have grain assemblages with greater than 50 percent of a weight or volume of particles smaller than 62.5 µm as mentioned in this paper.
References
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Book

The chemistry of clay minerals

TL;DR: Rich as mentioned in this paper discusses the relationship of composition to structure of layer silicates of clay and the relationship between weathering and electrochemica reactions to a smal degree in a series of books called "Developments in Sedimentology".
Book

Chemistry of clays and clay minerals

TL;DR: An overview of the chemical consititution and properties of clay minerals and the environmental conditions that lead to their formation is provided in this paper, where the authors provide a detailed view of the eight main groups of clays containing silica and non-siliceous oxide clays.
Journal ArticleDOI

Octahedral Occupancy and the Chemical Composition of Diagenetic (Low-Temperature) Chlorites

Stephen Hillier, +1 more
- 01 Jun 1991 - 
TL;DR: The chemical composition of 500 diagenetic chlorites, determined by electron microprobe, has been studied in six different sedimentary sequences spanning conditions from early diagenesis to low-grade metamorphism, in the temperature range 40-330°C.
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