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2018 | OriginalPaper | Buchkapitel

3. Geochemistry and Mineralogy

verfasst von : Neil Craigie

Erschienen in: Principles of Elemental Chemostratigraphy

Verlag: Springer International Publishing

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Abstract

Provided the data are considered to be of high quality (in terms of precision, accuracy, detection limits etc.), the mineralogical affinities of elements and controls on geochemistry and mineralogy should be understood before utilizing the inorganic geochemical data to propose chemostratigraphic schemes. Some elements are almost exclusive to particular minerals (e.g. Hf and Zr in zircons), but many are not. For example, Ti may be linked with a number of heavy minerals including rutile, anatase, sphene, titanomagnetite, magnetite and illmenite. Similarly, K is often concentrated in K feldspars, but may also be associated with clay minerals (e.g. illite) and micas. For this reason, it is necessary to gain an understanding of element:mineral links by comparing geochemical and mineralogical data acquired from the same samples, and by employing statistical and graphical techniques.

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Vorheriges Kapitel Sampling, Sample Preparation and Analytical Techniques
Nächstes Kapitel Production of Chemostratigraphic Correlation Schemes
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Metadaten
Titel
Geochemistry and Mineralogy
verfasst von
Neil Craigie
Copyright-Jahr
2018
Buch
Principles of Elemental Chemostratigraphy

Print ISBN: 978-3-319-71215-4

Electronic ISBN: 978-3-319-71216-1

Copyright-Jahr: 2018

DOI
https://doi.org/10.1007/978-3-319-71216-1_3