U–Th systematics of dispersed young volcanoes in NE China: Asthenosphere upwelling caused by piling up and upward thickening of stagnant Pacific slab

Author:

Zou Haibo,Fan Qicheng,Yao Yupeng

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference68 articles.

1. An analysis of variations in isentropic melt productivity;Asimow;Phil. Trans. R. Soc. Lond. A,1997

2. U-series isotope evidence for the origin of continental basalts;Asmerom;Earth Planet. Sci. Lett.,1995

3. Measurements of 232Th/230Th in volcanic rocks by PIMMS using the ThermoFinnigan Neptune;Ball,2002

4. Major element, REE, and Pb, Nd and Sr isotopic geochemistry of Cenozoic volcanic rocks of eastern China: implications for their origin from suboceanic-type mantle reservoirs;Basu;Earth Planet. Sci. Lett.,1991

5. Bourdon, B.P., 1994. Mass spectrometric measurements of U–Th disequilibrium in young volcanics: Implications for magmatic processes. Ph.D. thesis Thesis, Columbia Univ., New York.

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