A convection mechanism for explaining episodicity of magmatism and orogeny

Author:

Walzer Uwe

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference24 articles.

1. E. V. Artyushkov,Density differentiation on the core-mantle interface and gravity convection, Phys. Earth Planet. Int.2 (1970), 318?325.

2. V. V. Belousov,Ob osnovnykh zakonomernostyakh razvitiya kontinentov, Fizika Zemli, Moscow, No. 7 (1972), 67?79.

3. V. E. Chain,Grundprobleme der Zyklizität/Azyklizität (Kontinuum/Diskontinuum) erdgeschichtlicher Entwicklungsprozesse, Ber. deutsch. Ges. geol. Wiss. Berlin,A16 (1971).

4. R. Dearnley,Orogenic fold-belts and a hypothesis of earth evolution, Phys. Chem. Earth7 (1966). 1?114 (see his Fig. 1).

5. G. Gastil,The distribution of mineral dates in time and space, Amer. J. Sci.258 (1960), 1?35.

Cited by 5 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. A simple model of whole-mantle convection;Journal of Geophysical Research;1985

2. Thermal regime of the Earth's outer core;Pure and Applied Geophysics PAGEOPH;1981

3. Creep in geodynamic processes;Tectonophysics;1977-09

4. Thermal interaction of the core and the mantle and long-term behavior of the geomagnetic field;Journal of Geophysical Research;1977-04-10

5. References;Developments in Geotectonics;1976

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