Crystallization temperatures of tholeiite parental liquids: Implications for the existence of thermally driven mantle plumes

Special Paper of the Geological Society of America

Volumn 430, Issue , 2007, Pages 235-260

  Falloon, Trevor J ^a   Green, David H ^b   Danyushevsky, Leonid V ^a  

^a UNIVERSITY OF TASMANIA   (Australia)

^b AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Hawaii; Iceland; Kilauea; Mantle plumes; Mantle potential temperatures; MORB; Olivine; Peridotite melting experiments; Primary magmas; Reunion

Indexed keywords

BASALT; GLASS; MAGNESIA; MELTING; OCEANOGRAPHY; OLIVINE; SILICATE MINERALS; STRUCTURAL GEOLOGY; SUBMARINE GEOLOGY; THERMAL PLUMES;

HAWAII; ICELANDS; KILAUEA; MANTLE PLUME; MORB; POTENTIAL TEMPERATURE; PRIMARY MAGMAS; REUNION;

LIQUIDS;

CORE-MANTLE BOUNDARY; CRYSTALLIZATION; LHERZOLITE; MAGMATISM; MANTLE PLUME; MID-OCEAN RIDGE BASALT; OCEAN ISLAND BASALT; OLIVINE; PARTIAL MELTING; PHENOCRYST; POTENTIAL TEMPERATURE; THOLEIITE;

ATLANTIC OCEAN; EAST PACIFIC RISE; HAWAII [(ISL) HAWAIIAN ISLANDS]; HAWAII [UNITED STATES]; HAWAIIAN ISLANDS; ICELAND; KILAUEA; MASCARENE ISLANDS; MID-ATLANTIC RIDGE; PACIFIC OCEAN; REUNION; UNITED STATES;

EID: 67949089078     PISSN: 00721077     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2007.2430(12)     Document Type: Article

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