Transfer of mantle fluids to the lower continental crust: Constraints from mantle mineralogy and Moho temperature-Reference-Cited by-同舟云学术

Transfer of mantle fluids to the lower continental crust: Constraints from mantle mineralogy and Moho temperature

Published:1990-06 Issue:3-4 Volume:83 Page:249-261
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Bucher-Nurminen Kurt

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference35 articles.

1. Evidence for liquid immiscibility in the upper mantle;Amundsen;Nature (London),1987

2. Thermal structure of the lithosphere beneath the Norwegian-Danish basin and the Southern Baltic shield: a major transition zone;Balling;Terra Cognita,1985

3. Internally-consistent thermodynamic data for minerals in the system Na2OK2OCaOMgOFeO Fe2O3Al2O3SiO2TiO2H2OCO2;Berman;J. Petrol.,1988

4. Rifting of the Galicia margin: Crustal thinning and emplacement of mantle rocks on the seafloor;Boillot,1988

5. Fluids in the lithosphere, 1. Experimental constraints on CO2 transport in dunite and quartzite at elevated P-T conditions with implications for mantle and crustal decarbonation processes;Brenan;Earth Planet. Sci. Lett.,1988

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