High-temperature, low-/medium-pressure clockwise P-T paths and melting in the 
development of regional migmatites: The role of crustal thickening and repeated 
plutonism

Jung, S.

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High-temperature, low-/medium-pressure clockwise P-T paths and melting in the development of regional migmatites: The role of crustal thickening and repeated plutonism

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Jung, S.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Jung, S. (2000). High-temperature, low-/medium-pressure clockwise P-T paths and melting in the development of regional migmatites: The role of crustal thickening and repeated plutonism. Geological Journal, 35, 345-359.

引用: https://hdl.handle.net/11858/00-001M-0000-0014-94FA-5

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