Phase relations in carbonate component of carbonatized eclogite and peridotite along subduction and continental geotherms

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Phase relations in carbonate component of carbonatized eclogite and peridotite along subduction and continental geotherms. / Bekhtenova, Altyna; Shatskiy, Anton; Podborodnikov, Ivan V. et al.

In: Gondwana Research, Vol. 94, 06.2021, p. 186-200.

Research output: Contribution to journal › Article › peer-review

BibTeX

@article{64653854dea741efa38450d474215d2c,

title = "Phase relations in carbonate component of carbonatized eclogite and peridotite along subduction and continental geotherms",

abstract = "Phase relations in the carbonate constituent of mafic and ultramafic suites are decisive in the deep carbon cycle and partial melting in the Earth's mantle. Here we present an experimental study of phase relations in the “Na‑carbonatite” and “K‑carbonatite” systems, which represent the carbonate constituent of mantle eclogites and peridotites, respectively. The phase relations in the “Na‑carbonatite” system indicate that the carbonate constituent of the mafic suite consists of Na2Ca4(CO3)5 + dolomite + eitelite, Na2Mg(CO3)2, at shallow mantle pressures and changes to Na2Ca4(CO3)5 + magnesite at depths exceeding 170 km. At the same time, the “K‑carbonatite” system indicates that the carbonate constituent of the ultramafic suite consists of K2Mg(CO3)2 + dolomite + magnesite at shallow mantle pressures and changes to K2Mg(CO3)2 + magnesite + aragonite at depths exceeding 170–180 km. The “Na‑carbonatite” solidus is located near 850 °C / 3 GPa and 1100 °C / 6.5 GPa and has a Clapeyron slope of 14 MPa/°C. The “K‑carbonatite” solidus is situated near 825 °C / 3 GPa and 1000 °C / 6.5 GPa and has a Clapeyron slope of 20 MPa/°C. Both solidi are hotter than subduction geotherms. Consequently, under anhydrous conditions, the carbonate constituent of mafic and ultramafic suites can survive subduction into the deep mantle without melting. However, warming even to moderate temperatures corresponding to continental geotherms should be accompanied by partial melting yielding alkaline carbonatite melt.",

keywords = "Carbonatite, Deep carbon cycle, Double carbonates, Earth's mantle, Eclogite-CO, High-pressure experiment, Mantle partial melting, Peridotite-CO",

author = "Altyna Bekhtenova and Anton Shatskiy and Podborodnikov, {Ivan V.} and Arefiev, {Anton V.} and Litasov, {Konstantin D.}",

note = "Funding Information: We thank O.G. Safonov and the anonymous reviewer for their careful and constructive reviews and D.I. Rezvukhin for helpful comments. This study was done on the state assignment of IGM SB RAS and supported by RFBR No. 21-55-14001 . KDL was supported by the state assignment of IHPP RAS. The SEM and EDX studies of experimental samples were performed in the Analytical Center for multi-elemental and isotope research SB RAS. We are grateful to N.S. Karmanov and A.T. Titov for their help in the analytical works. Publisher Copyright: {\textcopyright} 2021 International Association for Gondwana Research Copyright: Copyright 2021 Elsevier B.V., All rights reserved.",

year = "2021",

month = jun,

doi = "10.1016/j.gr.2021.02.019",

language = "English",

volume = "94",

pages = "186--200",

journal = "Gondwana Research",

issn = "1342-937X",

publisher = "Elsevier Science Inc.",

}

RIS

TY - JOUR

T1 - Phase relations in carbonate component of carbonatized eclogite and peridotite along subduction and continental geotherms

AU - Bekhtenova, Altyna

AU - Shatskiy, Anton

AU - Podborodnikov, Ivan V.

AU - Arefiev, Anton V.

AU - Litasov, Konstantin D.

N1 - Funding Information: We thank O.G. Safonov and the anonymous reviewer for their careful and constructive reviews and D.I. Rezvukhin for helpful comments. This study was done on the state assignment of IGM SB RAS and supported by RFBR No. 21-55-14001 . KDL was supported by the state assignment of IHPP RAS. The SEM and EDX studies of experimental samples were performed in the Analytical Center for multi-elemental and isotope research SB RAS. We are grateful to N.S. Karmanov and A.T. Titov for their help in the analytical works. Publisher Copyright: © 2021 International Association for Gondwana Research Copyright: Copyright 2021 Elsevier B.V., All rights reserved.

PY - 2021/6

Y1 - 2021/6

N2 - Phase relations in the carbonate constituent of mafic and ultramafic suites are decisive in the deep carbon cycle and partial melting in the Earth's mantle. Here we present an experimental study of phase relations in the “Na‑carbonatite” and “K‑carbonatite” systems, which represent the carbonate constituent of mantle eclogites and peridotites, respectively. The phase relations in the “Na‑carbonatite” system indicate that the carbonate constituent of the mafic suite consists of Na2Ca4(CO3)5 + dolomite + eitelite, Na2Mg(CO3)2, at shallow mantle pressures and changes to Na2Ca4(CO3)5 + magnesite at depths exceeding 170 km. At the same time, the “K‑carbonatite” system indicates that the carbonate constituent of the ultramafic suite consists of K2Mg(CO3)2 + dolomite + magnesite at shallow mantle pressures and changes to K2Mg(CO3)2 + magnesite + aragonite at depths exceeding 170–180 km. The “Na‑carbonatite” solidus is located near 850 °C / 3 GPa and 1100 °C / 6.5 GPa and has a Clapeyron slope of 14 MPa/°C. The “K‑carbonatite” solidus is situated near 825 °C / 3 GPa and 1000 °C / 6.5 GPa and has a Clapeyron slope of 20 MPa/°C. Both solidi are hotter than subduction geotherms. Consequently, under anhydrous conditions, the carbonate constituent of mafic and ultramafic suites can survive subduction into the deep mantle without melting. However, warming even to moderate temperatures corresponding to continental geotherms should be accompanied by partial melting yielding alkaline carbonatite melt.

AB - Phase relations in the carbonate constituent of mafic and ultramafic suites are decisive in the deep carbon cycle and partial melting in the Earth's mantle. Here we present an experimental study of phase relations in the “Na‑carbonatite” and “K‑carbonatite” systems, which represent the carbonate constituent of mantle eclogites and peridotites, respectively. The phase relations in the “Na‑carbonatite” system indicate that the carbonate constituent of the mafic suite consists of Na2Ca4(CO3)5 + dolomite + eitelite, Na2Mg(CO3)2, at shallow mantle pressures and changes to Na2Ca4(CO3)5 + magnesite at depths exceeding 170 km. At the same time, the “K‑carbonatite” system indicates that the carbonate constituent of the ultramafic suite consists of K2Mg(CO3)2 + dolomite + magnesite at shallow mantle pressures and changes to K2Mg(CO3)2 + magnesite + aragonite at depths exceeding 170–180 km. The “Na‑carbonatite” solidus is located near 850 °C / 3 GPa and 1100 °C / 6.5 GPa and has a Clapeyron slope of 14 MPa/°C. The “K‑carbonatite” solidus is situated near 825 °C / 3 GPa and 1000 °C / 6.5 GPa and has a Clapeyron slope of 20 MPa/°C. Both solidi are hotter than subduction geotherms. Consequently, under anhydrous conditions, the carbonate constituent of mafic and ultramafic suites can survive subduction into the deep mantle without melting. However, warming even to moderate temperatures corresponding to continental geotherms should be accompanied by partial melting yielding alkaline carbonatite melt.

KW - Carbonatite

KW - Deep carbon cycle

KW - Double carbonates

KW - Earth's mantle

KW - Eclogite-CO

KW - High-pressure experiment

KW - Mantle partial melting

KW - Peridotite-CO

UR - http://www.scopus.com/inward/record.url?scp=85102886658&partnerID=8YFLogxK

U2 - 10.1016/j.gr.2021.02.019

DO - 10.1016/j.gr.2021.02.019

M3 - Article

AN - SCOPUS:85102886658

VL - 94

SP - 186

EP - 200

JO - Gondwana Research

JF - Gondwana Research

SN - 1342-937X

ER -

ID: 28143567