Carbonate in igneous and metamorphic fluorapatite: Two type A and two type B substitutions

American Mineralogist

Volumn 93, Issue 1, 2008, Pages 168-176

  Tacker, R Chris ^a  

^a NORTH CAROLINA MUSEUM OF NATURAL SCIENCES   (United States)

Author keywords

Analysis; Chemical (mineral); Crystal structure; IR spectroscopy; Pegmatites; Thermodynamics

Indexed keywords

APATITE; CARBON DIOXIDE; CARBONATION; CHEMICAL ANALYSIS; CRYSTAL STRUCTURE; CRYSTAL SYMMETRY; FOURIER TRANSFORM INFRARED SPECTROSCOPY; GRANITE; INFRARED SPECTROSCOPY; METAMORPHIC ROCKS; THERMODYNAMICS;

ANALYSIS; CARBONATE CONTENT; CRYSTAL STRUCTURAL; DIFFERENT MECHANISMS; FOURIER TRANSFORM INFRARED MICROSPECTROSCOPY; NATURALLY OCCURRING; PEGMATITES; THERMODYNAMIC CALCULATIONS;

CESIUM;

A-TYPE ROCK; CARBONATE; CHEMICAL ANALYSIS; CRYSTAL STRUCTURE; CRYSTALLOGRAPHY; FLUORAPATITE; FTIR SPECTROSCOPY; IGNEOUS ROCK; METAMORPHIC ROCK; SUBSTITUTION; SYMMETRY; THERMODYNAMICS;

EID: 38849147804     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2008.2551     Document Type: Article

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