Origin of Late Paleogene to Neogene basalts and associated coeval felsic volcanic rocks in Southwest Hokkaido, northern NE Japan arc: Constraints from Sr and Nd isotopes and major- and trace-element chemistry

Lithos

Volumn 125, Issue 1-2, 2011, Pages 368-392

  Takanashi, Koshiro ^a   Shuto, Kenji ^a   Sato, Makoto ^b  

^a NIIGATA UNIVERSITY   (Japan)

^b Nissaku Co Ltd   (Japan)

Author keywords

Asthenospheric upwelling; Basalt; Felsic volcanic rocks; Lower crust; Southwest Hokkaido; Sr Nd isotopes

Indexed keywords

AMPHIBOLITE; ASTHENOSPHERE; BASALT; DACITE; FELSIC ROCK; FRACTIONAL CRYSTALLIZATION; GABBRO; ISOTOPIC COMPOSITION; LOWER CRUST; MAFIC ROCK; MAGMA; MIOCENE; NEODYMIUM ISOTOPE; OLIGOCENE; PARTIAL MELTING; PLIOCENE; QUATERNARY; RARE EARTH ELEMENT; RHYOLITE; STRONTIUM ISOTOPE; TRACE ELEMENT; UPWELLING; VOLCANIC ROCK; VOLCANISM; XENOLITH;

HOKKAIDO; JAPAN; PACIFIC OCEAN; SEA OF JAPAN;

EID: 79958784253     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2011.02.020     Document Type: Article

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