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

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.

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Item Permalink: https://hdl.handle.net/11858/00-001M-0000-0014-94FA-5 Version Permalink: https://hdl.handle.net/11858/00-001M-0000-0014-94FB-3

Genre: Journal Article

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Creators:
Jung, S.¹, Author

Affiliations:
1Geochemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826288

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Dates: Date issued: 2000

Publication Status: Issued

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Identifiers: eDoc: 373169
Other: 26637

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Title: Geological Journal

Source Genre: Journal

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Pages: - Volume / Issue: 35 Sequence Number: - Start / End Page: 345 - 359 Identifier: -