Origin of the I- and S-type tonalite magma in the Satsunai-gawa Shichino-sawa river region of the Hidaka metamorphic belt, Hokkaido, northern Japan: Inferences from Sr and Nd isotopic compositions

Author:

Kojima Moeru1,Shimura Toshiaki

Affiliation:

1. Graduate School of Science and Engineering, Yamaguchi University

Publisher

The Geological Society of Japan

Subject

General Earth and Planetary Sciences,General Engineering,General Environmental Science

Reference72 articles.

1. Arth, J. G., 1976, Behaviour of trace elements during magmatic processes-a summary of theoretical models and their applications. Jour. Res. U. S. Geol. Surv., 4, 41-47.

2. Bea, F., Pereira, M. D. and Stroh, A., 1994, Mineral/leucosome trace-element partitioning in a peraluminous migmatite (a laser ablation-ICP-MS study). Chem. Geol., 117, 291-312.

3. Büsch, W., Schneider, G. and Mehnert, K. R., 1974, Initial melting at grain boundaries, Part II: Melting in rocks of granodioritic, quartzdioritic and tonalitic composition. Neues Jahrb. Mineral. Monatsh., 8, 345-370.

4. Blichert-Toft, J., Lesher, C. E. and Rosing, M. T., 1992, Selectively contaminated magmas of the Tertiary East Greenland macrodike complex. Contrib. Mineral. Petrol., 110, 154-172.

5. Chappell, B. W. and White, A. J. R., 1974, Two contrasting granite types. Pacific Geol., 8, 173-174.

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