Kimberlite genesis from a common carbonate-rich primary melt modified by lithospheric mantle assimilation-Reference-Cited by-同舟云学术

Kimberlite genesis from a common carbonate-rich primary melt modified by lithospheric mantle assimilation

Published:2020-04-24 Issue:17 Volume:6 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Giuliani Andrea¹²³^ORCID,Pearson D. Graham⁴^ORCID,Soltys Ashton¹^ORCID,Dalton Hayden¹^ORCID,Phillips David¹^ORCID,Foley Stephen F.²^ORCID,Lim Emilie¹^ORCID,Goemann Karsten⁵^ORCID,Griffin William L.²,Mitchell Roger H.⁶

Affiliation:

1. KiDs (Kimberlites and Diamonds), School of Earth Sciences, The University of Melbourne, Parkville, 3010 Victoria, Australia.

2. Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, North Ryde, 2109 New South Wales, Australia.

3. Institute of Geochemistry and Petrology, Department of Earth Sciences, ETH Zurich, Clausiusstrasse 25, Zurich 8092, Switzerland.

4. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada.

5. Central Science Laboratory, University of Tasmania, Hobart 7001 Tasmania, Australia.

6. Department of Geology, Lakehead University, P7B 5E1 Ontario, Canada.

Abstract

Diamond-bearing kimberlites were born from similar melts in the deep Earth and variably modified during ascent.

Funder

Australian Research Council

Swiss National Science Foundation

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference50 articles.

1. Superkimberlites: A geodynamic diamond window to the Earth's core

2. Hydrous mantle transition zone indicated by ringwoodite included within diamond

3. Stable isotope (C, O, S) compositions of volatile-rich minerals in kimberlites: A review

4. Instability of garnet from the mantle: Glass as evidence of metasomatic melting

5. Petrology of hypabyssal kimberlites: Relevance to primary magma compositions

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