CO2-Rich Melts in Earth

Gregory M. Yaxley; Sujoy Ghosh; Ekaterina S. Kiseeva; Ananya Mallik; Carl Spandler; Andrew R. Thomson; Michael J. Walter

CO₂-Rich Melts in Earth

Gregory M. Yaxley
, Sujoy Ghosh
, Ekaterina S. Kiseeva
, Ananya Mallik
, Carl Spandler
, Andrew R. Thomson
, Michael J. Walter

School of Biological, Earth and Environmental Sciences

Research output: Chapter in Book/Report/Conference proceedings › Chapter › peer-review

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.

Original language	English
Title of host publication	Deep Carbon
Subtitle of host publication	Past to Present
Publisher	Cambridge University Press
Pages	129-162
Number of pages	34
ISBN (Electronic)	9781108677950
ISBN (Print)	9781108477499
Publication status	Published - 1 Jan 2019

Keywords

Carbonate melt
Carbonate stability
Carbonatite
Cratonic
EMFDD
EMOG
Oxygen fugacity
Peridotite
Solidus
Subduction

Cite this

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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{\textquoteright}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.",

keywords = "Carbonate melt, Carbonate stability, Carbonatite, Cratonic, EMFDD, EMOG, Oxygen fugacity, Peridotite, Solidus, Subduction",

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T1 - CO2-Rich Melts in Earth

AU - Yaxley, Gregory M.

AU - Ghosh, Sujoy

AU - Kiseeva, Ekaterina S.

AU - Mallik, Ananya

AU - Spandler, Carl

AU - Thomson, Andrew R.

AU - Walter, Michael J.

N1 - Publisher Copyright: © Cambridge University Press 2020.

PY - 2019/1/1

Y1 - 2019/1/1

N2 - 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.

AB - 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.

KW - Carbonate melt

KW - Carbonate stability

KW - Carbonatite

KW - Cratonic

KW - EMFDD

KW - EMOG

KW - Oxygen fugacity

KW - Peridotite

KW - Solidus

KW - Subduction

UR - https://www.scopus.com/pages/publications/85081002360

M3 - Chapter

AN - SCOPUS:85081002360

SN - 9781108477499

SP - 129

EP - 162

BT - Deep Carbon

PB - Cambridge University Press

ER -

CO₂-Rich Melts in Earth

Abstract

Keywords

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