Walzer, Uwe (1974) A convection mechanism for explaining episodicity of magmatism and orogeny. Pure and Applied Geophysics PAGEOPH, 112. 106-117 doi:10.1007/bf00875924
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | A convection mechanism for explaining episodicity of magmatism and orogeny | ||
Journal | Pure and Applied Geophysics PAGEOPH | ||
Authors | Walzer, Uwe | Author | |
Year | 1974 | Volume | 112 |
Publisher | Springer Science and Business Media LLC | ||
DOI | doi:10.1007/bf00875924Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 1013045 | Long-form Identifier | mindat:1:5:1013045:6 |
GUID | 0 | ||
Full Reference | Walzer, Uwe (1974) A convection mechanism for explaining episodicity of magmatism and orogeny. Pure and Applied Geophysics PAGEOPH, 112. 106-117 doi:10.1007/bf00875924 | ||
Plain Text | Walzer, Uwe (1974) A convection mechanism for explaining episodicity of magmatism and orogeny. Pure and Applied Geophysics PAGEOPH, 112. 106-117 doi:10.1007/bf00875924 | ||
In | (1974) Pure and Applied Geophysics Vol. 112 (1) Springer Science and Business Media LLC |
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