Chemical substitutions, paragenetic relations, and physical conditions of formation of högbomite in the Sittampundi layered anorthosite complex, South India

American Mineralogist

Volumn 94, Issue 11-12, 2009, Pages 1520-1534

  Sengupta, Pulak ^a   Bhui, Uttam K ^a   Braun, Ingo ^b   Dutta, Upama ^a   Mukhopadhyay, D ^c  

^a JADAVPUR UNIVERSITY   (India)

^b UNIVERSITY OF BONN   (Germany)

^c UNIVERSITY OF CALCUTTA   (India)

Author keywords

Anorthosite; Corundum; H gbomite; Sittampundi; South India; Spinel; Ti mobility

Indexed keywords

BINARY ALLOYS; CALCITE; CHROMITE; CHROMITE DEPOSITS; CHROMIUM COMPOUNDS; CORUNDUM; CORUNDUM DEPOSITS; FELDSPAR; IGNEOUS ROCKS; II-VI SEMICONDUCTORS; IRON ALLOYS; IRON OXIDES; MAGNESIA; NICKEL OXIDE; OXIDE MINERALS; SILICATES; STRUCTURAL GEOLOGY; TITANIUM DIOXIDE; ZINC OXIDE;

ANORTHOSITE; SITTAMPUNDI; SOUTH INDIA; SPINEL; TI MOBILITIES;

GALLIUM COMPOUNDS;

AMPHIBOLITE FACIES; ANORTHOSITE; CHEMICAL COMPOSITION; CONCENTRATION (COMPOSITION); CORUNDUM; FELSIC ROCK; FLUID INCLUSION; FORMATION MECHANISM; GEOBAROMETRY; LAYERED INTRUSION; MAFIC ROCK; MOBILIZATION; PARAGENESIS; PYROXENITE; RETROGRADE METAMORPHISM; SPINEL; SUBSTITUTION;

INDIA;

EID: 77249084136     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2009.3121     Document Type: Article

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