Carbonate-chloride enrichment in fresh kimberlites of the Udachnaya-East pipe, Siberia: A clue to physical properties of kimberlite magmas?

Author:

Kamenetsky Vadim S.1,Kamenetsky Maya B.1,Sharygin Victor V.2,Golovin Alexander V.2

Affiliation:

1. Australian Research Council Centre of Excellence in Ore Deposits and School of Earth Sciences; University of Tasmania; Hobart, Tasmania Australia

2. Institute of Geology and Mineralogy; Siberian Branch of Russian Academy of Sciences; Novosibirsk Russia

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference35 articles.

1. Variations in chemical and isotopic compositions of the Yakutian kimberlites and their causes;Bogatikov;Geochem. Int.,2004

2. Garnet dissolution and the emplacement of kimberlites;Canil;Earth Planet. Sci. Lett.,1999

3. Kimberlites and Their Xenoliths

4. Physicochemical properties of alkali carbonatite lavas: Data from the 1988 eruption of Oldoinyo Lengai;Dawson;J. Geology.,1990

5. Evolution of natrocarbonatite from a wollastonite nephelinite parent: Evidence from the June, 1993, eruption of Oldoinyo Lengai, Tanzania;Dawson;J. Geol.,1996

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