Forsterite, hydrous and anhydrous wadsleyite and ringwoodite (Mg 2SiO4): 29Si NMR results for chemical shift anisotropy, spin-lattice relaxation, and mechanism of hydration

American Mineralogist

Volumn 94, Issue 7, 2009, Pages 905-915

  Stebbins, Jonathan F ^a   Smyth, Joseph R ^b   Panero, Wendy R ^c   Frost, Daniel J ^d  

^a STANFORD UNIVERSITY   (United States)

^b UNIVERSITY OF COLORADO   (United States)

^c OHIO STATE UNIVERSITY   (United States)

^d UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

Forsterite; Nmr spectroscopy; Ringwoodite; Wadsleyite; Water in mantle

Indexed keywords

ANISOTROPY; CHEMICAL SHIFT; EXPONENTIAL FUNCTIONS; NUCLEAR MAGNETIC RESONANCE SPECTROSCOPY; OLIVINE; PARAMAGNETISM; SILICON; SPECTROSCOPIC ANALYSIS; SPIN-LATTICE RELAXATION;

CHEMICAL SHIFT ANISOTROPY; FORSTERITES; PARAMAGNETIC IMPURITY; RINGWOODITE; SPECTROSCOPIC STUDIES; STRETCHED EXPONENTIAL FUNCTIONS; THEORETICAL CALCULATIONS; WADSLEYITE;

SILICON COMPOUNDS;

ANISOTROPY; FORSTERITE; HIGH TEMPERATURE; HYDRATION; LATTICE DYNAMICS; MAGNESIUM; MANTLE; NUCLEAR MAGNETIC RESONANCE; RINGWOODITE; VIBRATION; WADSLEYITE;

EID: 68949125373     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2009.3184     Document Type: Article

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