Mantle phlogopite: a significant lead repository?-Reference-Cited by-同舟云学术

Mantle phlogopite: a significant lead repository?

Published:1993-06 Issue:3-4 Volume:106 Page:475-483
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Rosenbaum Jeffrey M.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference26 articles.

1. Mantle metasomatism—continuing chemical change within the Earth;Bailey;Nature (London),1982

2. Pb, Nd, and Sr isotopic investigations of kaersutite and clinopyroxene from ultramafic nodules and their host basalts: The nature of the subcontinental mantle;Ben Othman;Geochim. Cosmochim. Acta,1990

3. Stable isotope, chemical, and petrographic studies of high-pressure amphiboles and micas: Evidence for metasomatism in the mantle source regions of alkali basalts and kimberlites;Boettcher;Am. J. Sci.,1980

4. Ultramafic nodules from the Kimberley pipes, South Africa;Boyd;Geochim. Cosmochim. Acta,1978

5. Primary and secondary phlogopites and clinopyroxenites in garnet lherzolite xenoliths;Carswell;Phys. Chem. Earth,1975

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