[ad_1]
Seifritz, W. CO2 disposal by means of silicates. Nature 345, 486–490 (1990).
Google Scholar
Lackner, K. S., Wendt, C. H., Butt, D. P., Joyce, E. L. & Sharp, D. H. Carbon dioxide disposal in carbonate minerals. Energy 20, 1153–1170 (1995).
Google Scholar
Oelkers, E. H., Gislason. S. R. & Matter. J. Mineral Carbonation of CO2. Elements 4, 333–337 (2008).
Matter, J. M. & Kelemen, P. B. Permanent storage of carbon dioxide in geological reservoirs by mineral carbonation. Nat. Geosci. 2, 837–841 (2009).
Google Scholar
Power, I. M. et al. Carbon mineralization: From natural analogues to engineered systems. Rev. Mineral. Geochem. 77, 305–360 (2013).
Google Scholar
Kelemen, P., Benson, S. M., Pilorgé, H., Psarras, P. & Wilcox, J. An overview of the status and challenges of CO2 storage in minerals and geological formations. Front. Clim. 1, 9 (2019).
Google Scholar
Pogge von Strandmann, P. A. E., Burton, K. W., Snæbjörnsdóttir, S. O., Sigfússon, B., Aradóttir, E. S., Gunnarsson, I. et al. Rapid CO2 mineralisation into calcite at the CarbFix storage site quantified using calcium isotopes. Nat. Commun. 10, 1983 (2019).
Snæbjörnsdóttir, S. Ó. et al. Carbon dioxide storage through mineral carbonation. Nat. Rev. Earth Environ. 1, 90–102 (2020).
Google Scholar
Rogers, K. L., Neuhoff, P. S., Pedersen, A. K. & Bird, D. K. CO2 metasomatism in a basalt-hosted petroleum reservoir, Nuussuaq, Weat Greenland. Lithos 92, 55–82 (2006).
Google Scholar
Goldberg, D. S., Takahashi, T. & Slagle, A. L. Carbon dioxide sequestration in deep-sea basalt. Proc. Natl. Acad. Sci. 105, 9920–9925 (2008).
Google Scholar
Shibuya, T. et al. Depth variation of carbon and oxygen isotopes of calcites in Archean altered upperoceanic crust: Implications for the CO2 flux from ocean to oceanic crust in the Archean. Earth Planet. Sci. Lett. 321–322, 64–73 (2012).
Google Scholar
Gislason, S. R. & Oelkers, E. H. Carbon storage in Basalt. Science 344, 373–374 (2014).
Google Scholar
Stockmann, G. J., Wolff-Boenisch, D., Gislason, S. R. & Oelkers, E. H. Do carbonate precipitates affect dissolution kinetics?. Chem. Geol. 337–338, 56–66 (2013).
Google Scholar
Monasterio-Guillot, L., Fernandez-Martinez, A., Ruiz-Agudo, E. & Rodriguez-Navarro, C. Carbonation of calcium-magnesium pyroxenes: Physical-chemical controls and effects of reaction-driven fracturing. Geochim. Cosmochim. Acta 304, 258–280 (2021).
Google Scholar
Berner, R. A., Sjoberg, E. L., Velbel, M. A. & Krom, M. D. Dissolution of pyroxenes and amphiboles during weathering. Science 80207, 1205–1206 (1980).
Google Scholar
Schott, J., Berner, R. A. & Sjoberg, E. L. Mechanism of pyroxene and amphibole weathering – I Experimental studies of iron-free minerals. Geochim. Cosmochim. Acta 45, 2123–2135 (1981).
Google Scholar
Petit, J.-C., Delia Mea, G., Dran, J.-C., Schott, J. & Berner, R. A. Mechanism of diopside dissolution from hydrogen depth profiling. Nature 325, 705–707 (1987).
Eggleston, C. M., Hochella, M. F. Jr. & Parks, G. A. Sample preparation and aging effects on the dissolution rate and surface composition of diopside. Geochim. Cosmochim. Acta 53, 797–804 (1989).
Google Scholar
Monasterio-Guillot, L., Rodriguez-Navarro, C. & Ruiz-Agudo, E. Kinetics and mechanisms of acid-pH weathering of pyroxenes. Geochem. Geophys. Geosyst. 22, e2021GC009711 (2021b).
Knauss, K. G., Nguyen, S. N. & Weed, H. C. Diopside dissolution kinetics as a function of pH, CO2, temperature, and time. Geochim. Cosmochim. Acta 57, 285–294 (1993).
Google Scholar
Chen, Y. & Brantley, S. L. Diopside and anthophyllite dissolution at 25° and 90°C and acid pH. Chem. Geol. 147, 233–248 (1998).
Google Scholar
Golubev, S. V., Pokrovsky, O. S. & Schott, J. Experimental determination of the effect of dissolved CO2 on the dissolution kinetics of Mg and Ca silicates at 25 °C. Chem. Geol. 217, 227–238 (2005).
Google Scholar
Dixit, S. & Carroll, S. A. Effect of solution saturation state and temperature on diopside dissolution. Geochem. Trans. 8, 3 (2007).
Google Scholar
Golubev, S. V. & Pokrovsky, O. S. Experimental study of the effect of organic ligands on diopside dissolution kinetics. Chem. Geol. 235, 377–389 (2006).
Google Scholar
Rigopoulos, I. et al. A method to enhance the CO2storage capacity of pyroxenitic rocks. Greenh. Gases Sci. Technol. 5, 577–591 (2015).
Google Scholar
Velde, B. Experimental pseudomorphism of diopside by talc and serpentine in (Ni, Mg)Cl2 aqueous solutions. Geochim. Cosmochim. Acta 52, 415–424 (1988).
Google Scholar
Majumdar, A. S., King, H. E., John, T., Kusebauch, C. & Putnis, A. Pseudomorphic replacement of diopside during interaction with (Ni, Mg)Cl2 aqueous solutions: Implications for the Ni-enrichment mechanism in talc- and serpentine-type phases. Chem. Geol. 380, 27–40 (2014).
Google Scholar
Austrheim, H. & Prestvik, T. Rodingitization and hydration of the oceanic lithosphere as developed in the Leka ophiolite, north–central Norway. Lithos 104, 177–198 (2008).
Google Scholar
Iyer, K., Austrheim, H., John, T. & Jamtveit, B. Serpentinization of the oceanic lithosphere and some geochemical consequences: Constraints from the Leka Ophiolite Complex, Norway. Chem. Geol. 249, 66–90 (2008).
Google Scholar
Alt, J. C. et al. The role of serpentinites in cycling of carbon and sulfur: Seafloor serpentinization and subduction metamorphism. Lithos 178, 40–54 (2013).
Google Scholar
Kelemen, P. B. & Matter, J. In situ carbonation of peridotite for CO2 storage. Proc. Natl. Acad. Sci. 105, 17295–17300 (2008).
Google Scholar
Falk, E. S. & Kelemen, P. B. Geochemistry and petrology of listvenite in the Samail ophiolite, Sultanate of Oman: Complete carbonation of peridotite during ophiolite emplacement. Geochim. Cosmochim. Acta 160, 70–90 (2015).
Google Scholar
de Obeso, J. C., Santiago Ramos, D. P., Higgins, J. A. & Kelemen, P. B. A Mg isotopic perspective on the mobility of magnesium during serpentinization and carbonation of the Oman ophiolite. J. Geophys. Res. Solid Earth 126, e2020JB020237 (2021).
Hansen, L. D., Dipple, G. M., Gordon, T. M. & Kellett, D. A. Carbonated serpentinite (listwanite) at Atlin, British Columbia: A geological analogue to carbon dioxide sequestration. Can. Mineral. 43, 225–239 (2005).
Google Scholar
Beinlich, A., Plümper, O., Hövelmann, J., Austrheim, H. & Jamtveit, B. Massive serpentinite carbonation at Linnajavri, N-Norway. Terra Nova 24, 446–455 (2012).
Google Scholar
Halls, C. & Zhao, R. Listvenite and related rocks: Perspectives on terminology and mineralogy with reference to an occurrence at Cregganbaun Co, Mayo, Republic of Ireland. Miner. Deposita 30, 303–313 (1995).
Google Scholar
Menzel, M. D. et al. Ductile deformation during carbonation of serpentinized peridotite. Nat. Commun. 13, 3478 (2022).
Google Scholar
Cutts, J. A., Steinthorsdottir, K., Turvey, C., Dipple, G. M., Enkin, R. J. & Peacock, S. M. Deducing mineralogy of serpentinized and carbonated ultramafic rocks using physical properties with implications for carbon sequestration and subduction zone dynamics. Geochem. Geophys. Geosyst. 22, e2021GC009989 (2021).
Schwarzenbach, E. M., Früh-Green, G. L., Bernasconi, S. M., Alt, J. C. & Plas, A. Serpentinization and carbon sequestration: A study of two ancient peridotite-hosted hydrothermal systems. Chem. Geol. 351, 115–133 (2013).
Google Scholar
Steele, A. et al. Organic synthesis associated with serpentinization and carbonation on early Mars. Science 375, 172–177 (2022).
Google Scholar
Yu, S. Y. et al. Tectono-thermal evolution of the Qilian orogenic system: Tracing the subduction, accretion and closure of the Proto-Tethys Ocean. Earth Sci. Rev. 215, 103547 (2021).
Google Scholar
Zhang, J., Yu, S. & Mattinson, C. G. Early Paleozoic polyphase metamorphism in northern Tibet, China. Gondwana Res. 41, 267–289 (2017).
Google Scholar
Li, X. W. et al. Geological structure characteristics and fluid activity of the gold-bearing quartz veins on the Yushishan Area, North Altyn Tagh. Geotectonica et Metallogenia (2020).
Liu, J. H. et al. Characteristics and formation of corundum within syenite in the Yushishan rare metal deposits in the northeastern Tibetan Plateau. American Mineralogist, accepted (2022). https://doi.org/10.2138/am-2022-8223.
Liu, T. & Jiang, S. Y. Multiple generations of tourmaline from Yushishanxi leucogranite in South Qilian of western China record a complex formation history from B-rich melt to hydrothermal fluid. Am. Miner. 106, 994–1008 (2021).
Google Scholar
Liu, T. et al. Titanite U-Pb dating and geochemical constraints on the Paleozoic magmatic-metamorphic events and Nb-Ta mineralization in the Yushishan deposit, South Qilian, NW China. Lithos 412–413, 106612 (2022).
Google Scholar
McDonough, W. F. & Sun, S.-S. The composition of the Earth. Chem. Geol. 120, 223–253 (1995).
Google Scholar
Morimoto, N. et al. Nomenclature of pyroxenes. Mineral. J. 14, 198–221 (1989).
Google Scholar
Python, M., Yoshikawa, M., Shibata, T. & Arai, S. Diopsidites and rodingites: Serpentinisation and Ca-metasomatism in the Oman ophiolite mantle. In Dyke Swarms: Keys for Geodynamic Interpretation (ed. Srivastava, R. K.) 401–435 (Springer, 2011).
Google Scholar
Lee, C.-T.A. & Lackey, J. S. Global continental arc flare-ups and their relation to long-term greenhouse conditions. Elements 11, 125–130 (2015).
Google Scholar
Python, M., Ceuleneer, G., Ishida, Y., Barrat, J.-A. & Arai, S. Oman diopsidites: A new lithology diagnostic of very high temperature hydrothermal circulation in mantle peridotite below oceanic spreading centres. Earth Planet. Sci. Lett. 255, 289–305 (2007).
Google Scholar
Akizawa, N. et al. High-temperature hydrothermal activities around suboceanic Moho: An example from diopsidite and anorthosite in Wadi Fizh, Oman ophiolite. Lithos 263, 66–87 (2016).
Google Scholar
Bach, W. & Klein, F. The petrology of seafloor rodingites: insights from geochemical reaction path modeling. Lithos 112, 103–117 (2009).
Google Scholar
Gong, X. K. et al. The determination of Triassic ultramafic-syenite intrusive body and its geological significance, western North Qinling. Acta Petrologica Sinica 32, 177–192 (2016).
Google Scholar
Dyer, B., Lee, C.-T.A., Leeman, W. P. & Tice, M. Open-system behavior during pluton-wall-rock interaction as constrained from a study of Endoskarns in the Sierra Nevada Batholith, California. J. Petrol. 52, 1987–2008 (2011).
Google Scholar
Ferry, J. M. Prograde and retrograde fluid flow during contact metamorphism of siliceous carbonate rocks from the Ballachulish aureole, Scotland. Contrib. Mineral Petrol. 124, 235–254 (1996).
Google Scholar
Ferry, J. M., Ushikubo, T. & Valley, J. W. Formation of forsterite by silicification of dolomite during contact metamorphism. J. Petrol. 52, 1619–1640 (2011).
Google Scholar
Proyer, A., Mposkos, E., Baziotis, I. & Hoinkes, G. Tracing high-pressure metamorphism in marbles: Phase relations in high-grade aluminous calcite–dolomite marbles from the Greek Rhodope massif in the system CaO–MgO–Al2O3–SiO2–CO2 and indications of prior aragonite. Lithos 104, 119–130 (2008).
Google Scholar
Ferrando, S., Groppo, C., Frezzotti, M. L., Castelli, D. & Proyer, A. Dissolving dolomite in a stable UHP mineral assemblage: Evidence from Cal-Dol marbles of the Dora-Maira Massif (Italian Western Alps). Am. Miner. 102, 42–60 (2017).
Google Scholar
Velbel, M. A. Dissolution of olivine during natural weathering. Geochim. Cosmochim. Acta 73, 6098–6113 (2009).
Google Scholar
Peuble, S. et al. Carbonate mineralization in percolated olivine aggregates: Linking effects of crystallographic orientation and fluid flow. Am. Mineralogist 100, 474–482 (2015).
Google Scholar
Phillips-Lander, C. M., Legett, C., Elwood Madden, A. S. & Elwood Madden, M. E. Can we use pyroxene weathering textures to interpret aqueous alteration conditions? Yes and No. Am. Mineralogist 102, 1915–1921 (2017).
Xia, F. et al. Mechanism and kinetics of pseudomorphic mineral replacement reactions: A case study of the replacement of pentlandite by violarite. Geochim. Cosmochim. Acta 73, 1945–1969 (2009).
Google Scholar
Putnis, A. Mineral replacement reactions. Rev. Mineral. Geochem. 70, 87–124 (2009).
Google Scholar
Putnis, A. Why mineral interfaces matter. Science 343, 1441–1442 (2014).
Google Scholar
Ruiz-Agudo, E. et al. Control of silicate weathering by interface-coupled dissolution-precipitation processes at the mineral-solution interface. Geology 44, 567–570 (2016).
Google Scholar
Rudge, J. F., Kelemen, P. B. & Spiegelman, M. A simple model of reaction-induced cracking applied to serpentinization and carbonation of peridotite. Earth Planet. Sci. Lett. 291, 215–227 (2010).
Google Scholar
Plümper, O., Røyne, A., Magrasó, A. & Jamtveit, B. The interface-scale mechanism of reaction-induced fracturing during serpentinization. Geology 40, 1103–1106 (2012).
Google Scholar
Malvoisin, B., Brantut, N. & Kaczmarek, M.-A. Control of serpentinisation rate by reaction-induced cracking. Earth Planet. Sci. Lett. 476, 143–152 (2017).
Google Scholar
Evans, O., Spiegelman, M. & Kelemen, P. B. Phase-field modeling of reaction-driven cracking: determining conditions for extensive olivine serpentinization. J. Geophys. Res. Solid Earth 125, e2019JB018614 (2020).
Guillot, S., Schwartz, S., Reynard, B., Agard, P. & Prigent, C. Tectonic significance of serpentinites. Tectonophysics 646, 1–19 (2015).
Google Scholar
Rouméjon, S., Andreani, M. & Früh-Green, G. L. Antigorite crystallization during oceanic retrograde serpentinization of abyssal peridotites. Contrib. Miner. Petrol. 174, 60 (2019).
Google Scholar
Schwartz, S. et al. Pressure–temperature estimates of the lizardite/antigorite transition in high pressure serpentinites. Lithos 178, 197–210 (2013).
Google Scholar
Kodolányi, J. & Pettke, T. Loss of trace elements from serpentinites during fluid-assisted transformation of chrysotile to antigorite — An example from Guatemala. Chem. Geol. 284, 351–362 (2011).
Google Scholar
Coleman, R. G. & Keith, T. E. A chemical study of serpentinization—Burro Mountain, California. J. Petrol. 12, 311–328 (1971).
Google Scholar
Deschamps, F., Godard, M., Guillot, S. & Hattori, K. Geochemistry of subduction zone serpentinites: A review. Lithos 178, 96–127 (2013).
Google Scholar
Nasir, S., Al Sayigh, A. R., Al Harthy, A., Al-Khirbash, S., Al-Jaaidi, O., Musllam, A. et al. Mineralogical and geochemical characterization of listwaenite from the Semail Ophiolite, Oman. Chemie Der Erde – Geochemistry 67, 213–228 (2007).
Malvoisin, B. Mass transfer in the oceanic lithosphere: Serpentinization is not isochemical. Earth Planet. Sci. Lett. 430, 75–85 (2015).
Google Scholar
Beinlich, A., Austrheim, H., Glodny, J., Erambert, M. & Andersen, T. B. CO2 sequestration and extreme Mg depletion in serpentinized peridotite clasts from the Devonian Solund basin, SN-Norway. Geochim. Cosmochim. Acta 74, 6935–6964 (2010).
Google Scholar
de Obeso, J. C. & Kelemen, P. B. Major element mobility during serpentinization, oxidation and weathering of mantle peridotite at low temperatures. Phil. Trans. R. Soc. A. 378, 20180433 (2020).
Google Scholar
Palandri, J. L. & Reed, M. H. Geochemical models of metasomatism in ultramafic systems: Serpentinization, rodingitization, and sea floor carbonate chimney precipitation. Geochim. Cosmochim. Acta 68, 1115–1133 (2004).
Google Scholar
Godard, M., Carter, E. J., Decrausaz, T., Lafay, R., Bennett, E., Kourim, F., de Obeso, J.-C., Michibayashi, K., Harris, M., Coggon, J. A., Teagle, D. A. H., Kelemen, P. B. & the Oman Drilling Project Phase 1 Science Party Geochemical profiles across the listvenite-metamorphic transition in the basal megathrust of the Semail ophiolite: Results from drilling at Oman DP Hole BT1B. J. Geophys. Res. Solid Earth 126(12), e2021JB022733 (2021). https://doi.org/10.1029/2021JB022733.
Monnier, C., Girardeau, J., Le Mée, L. & Polvé, M. Along-ridge petrological segmentation of the mantle in the Oman ophiolite. Geochem. Geophys. Geosyst. 7, Q11008 (2006).
Google Scholar
Schwarzenbach, E. M., Vogel, M., Früh-Green, G. L. & Boschi, C. Serpentinization, carbonation and metasomatism of ultramafic sequences in the Northern Apennine ophiolite (NW Italy). J. Geophys. Res. Solid Earth 126, e2020JB020619 (2021).
Frisby, C., Bizimis, M. & Mallick, S. Hf–Nd isotope decoupling in bulk abyssal peridotites due to serpentinization. Chem. Geol. 440, 60–72 (2016).
Google Scholar
Frisby, C., Bizimis, M. & Mallick, S. Seawater-derived rare earth element addition to abyssal peridotites during serpentinization. Lithos 248–251, 432–454 (2016).
Google Scholar
Peters, D., Bretscher, A., John, T., Scambelluri, M. & Pettke, T. Fluid-mobile elements in serpentinites: Constraints on serpentinisation environments and element cycling in subduction zones. Chem. Geol. 466, 654–666 (2017).
Google Scholar
Raza, A., Glatz, G., Gholami, F., Mahmoud, M. & Alafnan, S. Carbon mineralization and geological storage of CO2 in basalt: Mechanisms and technical challenges. Earth Sci. Rev. 229, 104036 (2022).
Google Scholar
Aradóttir, E. S. P., Sonnenthal, E. L., Björnsson, G. & Jónsson, H. Multidimensional reactive transport modeling of CO2 mineral sequestration in basalts at the Hellisheidi geothermal field, Iceland. Int. J. Greenhouse Gas Control 9, 24–40 (2012).
Google Scholar
McGrail, B. P., Spane, F. A., Amonette, J. E., Thompson, C. R. & Brown, C. F. Injection and monitoring at the Wallula basalt pilot project. Energy Procedia 63, 2939–2948 (2014).
Google Scholar
Wen, G., Li, J.-W., Hofstra, A. H., Koenig, A. E. & Cui, B.-Z. Textures and compositions of clinopyroxene in an Fe skarn with implications for ore-fluid evolution and mineral-fluid REE partitioning. Geochim. Cosmochim. Acta 290, 104–123 (2020).
Google Scholar
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