On a systematic error in the X-ray determination of octahedral Fe and Mg in biotites

P. K. Hörmann; G. Morteani

doi:10.1007/BF00400131

On a systematic error in the X-ray determination of octahedral Fe and Mg in biotites

P. K. Hörmann
, G. Morteani

Christian-Albrechts-Universitat zu Kiel

Research output: Contribution to journal › Article › peer-review

1 Scopus citations

Abstract

A systematic error in the determination of the Fe, Mg contents of biotites by X-ray intensity measurements of the 001 reflections by the Franzini and Schiaffino-method is investigated. It was found that the results are strongly influenced by the number of vacancises within the octahedral layer, and in the interlayer of the investigated biotites.

Original language	English
Pages (from-to)	368-374
Number of pages	7
Journal	Contributions to Mineralogy and Petrology
Volume	22
Issue number	4
DOIs	https://doi.org/10.1007/BF00400131
State	Published - Jun 1969
Externally published	Yes

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10.1007/BF00400131

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title = "On a systematic error in the X-ray determination of octahedral Fe and Mg in biotites",

abstract = "A systematic error in the determination of the Fe, Mg contents of biotites by X-ray intensity measurements of the 001 reflections by the Franzini and Schiaffino-method is investigated. It was found that the results are strongly influenced by the number of vacancises within the octahedral layer, and in the interlayer of the investigated biotites.",

author = "H{\"o}rmann, \{P. K.\} and G. Morteani",

year = "1969",

month = jun,

doi = "10.1007/BF00400131",

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journal = "Contributions to Mineralogy and Petrology",

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T1 - On a systematic error in the X-ray determination of octahedral Fe and Mg in biotites

AU - Hörmann, P. K.

AU - Morteani, G.

PY - 1969/6

Y1 - 1969/6

N2 - A systematic error in the determination of the Fe, Mg contents of biotites by X-ray intensity measurements of the 001 reflections by the Franzini and Schiaffino-method is investigated. It was found that the results are strongly influenced by the number of vacancises within the octahedral layer, and in the interlayer of the investigated biotites.

AB - A systematic error in the determination of the Fe, Mg contents of biotites by X-ray intensity measurements of the 001 reflections by the Franzini and Schiaffino-method is investigated. It was found that the results are strongly influenced by the number of vacancises within the octahedral layer, and in the interlayer of the investigated biotites.

UR - https://www.scopus.com/pages/publications/34250489366

U2 - 10.1007/BF00400131

DO - 10.1007/BF00400131

M3 - Article

AN - SCOPUS:34250489366

SN - 0010-7999

VL - 22

SP - 368

EP - 374

JO - Contributions to Mineralogy and Petrology

JF - Contributions to Mineralogy and Petrology

IS - 4

ER -

On a systematic error in the X-ray determination of octahedral Fe and Mg in biotites

Abstract

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