Optimal spectrum, site occupancy, and oxidation state of Mn in montmorillonite

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Authors:Sherman, David M.; Vergo, Norma
Author Affiliations:Primary:
U. S. Geol. Surv., Reston, VA, United States
Volume Title:American Mineralogist
Source:American Mineralogist, 73(1-2), p.140-144. Publisher: Mineralogical Society of America, Washington, DC, United States. ISSN: 0003-004X
Publication Date:1988
Note:In English. 17 refs.; illus. incl. 4 tables
Summary:Optical (diffuse-reflectance) spectra are used to characterize the crystal chemistry of Mn in pegmatite-associated montmorillonite. The Mn is present as Mn3+. [J.A.Z.]
Subjects:Clay mineralogy; Clay minerals; Crystal chemistry; Experimental studies; Granites; Igneous rocks; Manganese; Metals; Mineral data; Minerals; Montmorillonite; Optical spectra; Oxidation; Pegmatite; Plutonic rocks; Sheet silicates; Silicates; Spectra
Abstract Numbers:88M/4977
Record ID:1988027965
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
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040 |a ViAlAGI  |c ViAlAGI 
072 7 |a 01B  |2 georeft 
100 1 |a Sherman, David M.  |e analytic author  |u U. S. Geol. Surv., Reston, VA 
245 1 0 |a Optimal spectrum, site occupancy, and oxidation state of Mn in montmorillonite 
300 |a p. 140-144 
500 |a In English. 17 refs. 
500 |a Abstract number: 88M/4977 
500 |a Abstractor: J.A.Z. 
500 |a Affiliation: U. S. Geol. Surv.; Reston, VA; USA; United States 
500 |a Key title: American Mineralogist 
500 |a Source note: American Mineralogist, 73(1-2), p.140-144. Publisher: Mineralogical Society of America, Washington, DC, United States. ISSN: 0003-004X 
500 |a Publication type: journal article 
504 |b 17 refs. 
510 3 |a GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom 
520 |a Optical (diffuse-reflectance) spectra are used to characterize the crystal chemistry of Mn in pegmatite-associated montmorillonite. The Mn is present as Mn>3+`. 
650 7 |a Clay mineralogy  |2 georeft 
650 7 |a Clay minerals  |2 georeft 
650 7 |a Crystal chemistry  |2 georeft 
650 7 |a Experimental studies  |2 georeft 
650 7 |a Granites  |2 georeft 
650 7 |a Igneous rocks  |2 georeft 
650 7 |a Manganese  |2 georeft 
650 7 |a Metals  |2 georeft 
650 7 |a Mineral data  |2 georeft 
650 7 |a Minerals  |2 georeft 
650 7 |a Montmorillonite  |2 georeft 
650 7 |a Optical spectra  |2 georeft 
650 7 |a Oxidation  |2 georeft 
650 7 |a Pegmatite  |2 georeft 
650 7 |a Plutonic rocks  |2 georeft 
650 7 |a Sheet silicates  |2 georeft 
650 7 |a Silicates  |2 georeft 
650 7 |a Spectra  |2 georeft 
700 1 |a Vergo, Norma,  |e analytic author 
773 0 |t American Mineralogist  |d Washington, DC : Mineralogical Society of America, Feb. 1988  |x 0003-004X  |y AMMIAY  |n American Mineralogist, 73(1-2), p.140-144. Publisher: Mineralogical Society of America, Washington, DC, United States. ISSN: 0003-004X Publication type: journal article  |g Vol. 73, no. 1-2  |h illus. incl. 4 tables