Noble gas isotopes in corundum and peridotite xenoliths from the eastern North China Craton: Implication for comprehensive refertilization of lithospheric mantle

Physics of the Earth and Planetary Interiors

Volumn 189, Issue 3-4, 2011, Pages 185-191

  He, Huaiyu ^a   Zhu, Rixiang ^a   Saxton, John ^b  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b NU INSTRUMENTS LTD   (United Kingdom)

Author keywords

Corundum; Helium isotope; North China Craton; Peridotite xenoliths; Titanomagnetite megacrystal

Indexed keywords

CHANGLE; CO-EXISTING; CORRELATION DIAGRAMS; HELIUM ISOTOPE; ISOTOPIC RATIOS; LITHOSPHERIC MANTLE; MANTLE XENOLITHS; NOBLE GAS; NOBLE GAS ISOTOPES; NORTH CHINA CRATON; PERIDOTITE XENOLITHS; SUBCONTINENTAL MANTLE; TAN LU FAULT ZONE; TITANOMAGNETITES; VOLCANIC FIELD; WEHRLITE;

CORUNDUM; HELIUM; LITHOLOGY; OLIVINE; STRUCTURAL GEOLOGY;

ISOTOPES;

ASTHENOSPHERE; CORUNDUM; FAULT ZONE; GEOCHEMISTRY; HELIUM ISOTOPE; ISOTOPIC COMPOSITION; ISOTOPIC RATIO; LHERZOLITE; MANTLE STRUCTURE; MEGACRYST; PERIDOTITE; PYROXENITE; TITANOMAGNETITE; WEHRLITE; XENOLITH;

CHINA; NORTH CHINA BLOCK;

EID: 82355169028     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2011.09.001     Document Type: Article

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