CO2-rich melts in Earth

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CO2-rich melts in Earth

Yaxley, Gregory M.; Ghosh, Sujoy; Kiseeva, Ekaterina S.; Mallik, Ananya; Spandler, Carl; Thomson, Andrew R.; Walter, Michael J.
Date: 2019-10
Copyright: © Cambridge University Press 2020. The online version of this work is published at doi.org/10.1017/9781108677950 under a Creative Commons Open Access license CC-BY-NC-SA 4.0 which permits re-use, distribution and reproduction in any medium for non-commercial purposes providing appropriate credit to the original work is given, any changes made are indicated, and the new work is published under the same license terms. To view a copy of this license, visit https://creativecommons.org/licenses/by-nc-sa/4.0 All versions of this work may contain content reproduced under license from third parties. Permission to reproduce this third-party content must be obtained from these third parties directly. When citing this work, please include a reference to the DOI 10.1017/9781108677950
Copyright information: https://creativecommons.org/licenses/by-nc-sa/4.0
Citation: Yaxley, G. M., Ghosh, S., Kiseeva, E. S., Mallik, A., Spandler, C., Thomson, A. R. and Walter, M. J. (2019) 'CO2-Rich Melts in Earth', in Orcutt, B.N., Daniel, I. & Dasgupta, R. (eds.) Deep Carbon: Past to Present. Cambridge: Cambridge University Press, pp. 129-162. doi: 10.1017/9781108677950.006
Published Version: 10.1017/9781108677950.006

Abstract:

This chapter reviews the systematics of partial melting of mantle lithologies – like peridotite and eclogite – in the presence of carbon dioxide. It discusses the composition of mantle-derived magmas generated in the presence of carbon dioxide and whether magmas erupted on Earth’s surface resemble carbonated magmas from the mantle. It reviews how the production of carbon dioxide-rich magma in the mantle varies as a function of tectonic settings – beneath continents and oceans and in subduction zones – and time.

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© Cambridge University Press 2020. The online version of this work is published at doi.org/10.1017/9781108677950 under a Creative Commons Open Access license CC-BY-NC-SA 4.0 which permits re-use, distribution and reproduction in any medium for non-commercial purposes providing appropriate credit to the original work is given, any changes made are indicated, and the new work is published under the same license terms. To view a copy of this license, visit https://creativecommons.org/licenses/by-nc-sa/4.0 All versions of this work may contain content reproduced under license from third parties. Permission to reproduce this third-party content must be obtained from these third parties directly. When citing this work, please include a reference to the DOI 10.1017/9781108677950 Except where otherwise noted, this item's license is described as © Cambridge University Press 2020. The online version of this work is published at doi.org/10.1017/9781108677950 under a Creative Commons Open Access license CC-BY-NC-SA 4.0 which permits re-use, distribution and reproduction in any medium for non-commercial purposes providing appropriate credit to the original work is given, any changes made are indicated, and the new work is published under the same license terms. To view a copy of this license, visit https://creativecommons.org/licenses/by-nc-sa/4.0 All versions of this work may contain content reproduced under license from third parties. Permission to reproduce this third-party content must be obtained from these third parties directly. When citing this work, please include a reference to the DOI 10.1017/9781108677950
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