Water solubility in coesite at realistic temperatures o8f subduction zones
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Weidong Sun | M. Lv | Wei Yan | Mingyue He | Xi Liu | Dan Wu | Xiaohu Li
[1] Xi Liu,et al. Effect of second Si–O vibrational overtones/combinations on quantifying water in silicate and silica minerals using infrared spectroscopy, and an experimental method for its removal , 2022, Physics and Chemistry of Minerals.
[2] Wei-dong Sun,et al. Experimental constraints on trace element partitioning between coesite and hydrous silicate melt at 5 GPa and 1500–1750°C , 2021, Science China Earth Sciences.
[3] T. Katsura,et al. Independent hydrogen incorporation in wadsleyite from oxygen fugacity and non-dissociation of H2O in the reducing mantle transition zone , 2021 .
[4] Wei-dong Sun,et al. Water in coesite: Incorporation mechanism and operation condition, solubility and P-T dependence, and contribution to water transport and coesite preservation , 2021 .
[5] Yong Zheng,et al. Two styles of plate tectonics in Earth's history. , 2020, Science bulletin.
[6] J. Smyth,et al. Crystal structures and high-temperature vibrational spectra for synthetic boron and aluminum doped hydrous coesite , 2019, Crystals.
[7] Lifei Zhang,et al. Ultrahigh‐pressure and high‐P lawsonite eclogites in Muzhaerte, Chinese western Tianshan , 2019, Journal of Metamorphic Geology.
[8] Weide Yan,et al. Fundamental infrared absorption features of α-quartz: An unpolarized single-crystal absorption infrared spectroscopic study , 2019, Vibrational Spectroscopy.
[9] A. Miyake,et al. Significance of an amorphous SiO2 phase in a pseudomorph after coesite enclosed in garnet from ultrahigh‐pressure eclogite, Su–Lu Belt, eastern China , 2018 .
[10] R. Stalder,et al. OH defects in coesite and stishovite during ultrahigh-pressure metamorphism of continental crust , 2018, Physics and Chemistry of Minerals.
[11] Xi Liu,et al. Some IR features of SiO 4 and OH in coesite, and its amorphization and dehydration at ambient pressure , 2017 .
[12] D. Frost,et al. Hydrous melting and partitioning in and above the mantle transition zone: Insights from water-rich MgO–SiO2–H2O experiments , 2017 .
[13] Xiaozhi Yang. Effect of oxygen fugacity on OH dissolution in olivine under peridotite-saturated conditions: an experimental study at 1.5-7 GPa and 1100-1300 °C , 2016 .
[14] H. Qian. High Temperature Stable Assembly Designed for Cubic Press , 2014 .
[15] D. C. Presnall. Phase Diagrams of Earth‐Forming Minerals , 2013 .
[16] H. Green,et al. Petrofabric and strength of SiO2 near the quartz‐coesite phase boundary , 2012 .
[17] R. Stalder,et al. OH defects in quartz in the system quartz–albite–water and granite–water between 5 and 25 kbar , 2012, Physics and Chemistry of Minerals.
[18] F. Peng,et al. A large volume cubic press with a pressure-generating capability up to about 10 GPa , 2012 .
[19] K. Fischer,et al. he global range of subduction zone thermal models , 2010 .
[20] R. Wirth,et al. IR calibrations for water determination in olivine, r-GeO2, and SiO2 polymorphs , 2009 .
[21] M. Koch-Müller,et al. Coupled boron and hydrogen incorporation in coesite , 2009 .
[22] S. Yoshioka,et al. Seismological and experimental constraints on metastable phase transformations and rheology of the Mariana slab , 2008 .
[23] M. Sambridge,et al. Quantitative absorbance spectroscopy with unpolarized light: Part II. Experimental evaluation and development of a protocol for quantitative analysis of mineral IR spectra , 2008 .
[24] M. Sambridge,et al. Quantitative absorbance spectroscopy with unpolarized light: Part I. Physical and mathematical development , 2008 .
[25] Gnoncr R. RossvraN,et al. Hydroxyl contents of accessory minerals in mantle eclogites and related rocks , 2007 .
[26] S. Nakashima,et al. Water content in natural eclogite and implication for water transport into the deep upper mantle , 2006 .
[27] J. Smyth,et al. Factors in the preservation of coesite: The importance of fluid inflitration , 2005 .
[28] W. Westrenen,et al. The influence of OH in coesite on the kinetics of the coesite-quartz phase transition , 2005 .
[29] Y. Fei,et al. OH– in synthetic and natural coesite , 2003 .
[30] I. Daniel,et al. Kinetics of the Coesite–Quartz Transition: Application to the Exhumation of Ultrahigh-Pressure Rocks , 2003 .
[31] Y. Nagano. Standard enthalpy of formation of platinic acid , 2002 .
[32] S. Maruyama,et al. Overpressures induced by coesite-quartz transition in zircon , 2001 .
[33] E. Hauri,et al. Location and quantitative analysis of OH in coesite , 2001 .
[34] J. Mosenfelder. Pressure dependence of hydroxyl solubility in coesite , 2000 .
[35] T. Nishiyama. Kinetic modeling of the coesite–quartz transition in an elastic field and its implication for the exhumation of ultrahigh‐pressure metamorphic rocks , 1998 .
[36] T. Reinecke. Prograde high- to ultrahigh-pressure metamorphism and exhumation of oceanic sediments at Lago di Cignana, Zermatt-Saas Zone, western Alps , 1998 .
[37] J. Mosenfelder,et al. Kinetics of the coesite to quartz transformation , 1997 .
[38] H. Keppler,et al. Water solubility in pyrope to 100 kbar , 1997 .
[39] J. Liou,et al. Occurrences of intergranular coesite in ultrahigh-P rocks from the Sulu region, eastern China: Implications for lack of fluid during exhumation , 1996 .
[40] W. Ernst,et al. Stability of hydrous phases in subducting oceanic crust , 1996 .
[41] R. Y. Zhang,et al. Coesite inclusions in dolomite from eclogite in the southern Dabie Mountains, China: The significance of carbonate minerals in UHPM rocks , 1996 .
[42] A. Okay,et al. A coesite inclusion in dolomite in Dabie Shan, China; petrological and rheological significance , 1994 .
[43] K. Pitzer,et al. EQUATIONS OF STATE VALID CONTINUOUSLY FROM ZERO TO EXTREME PRESSURES FOR H2O AND CO2 , 1994 .
[44] G. Libourel,et al. Boron partitioning in the upper mantle: An experimental and ion probe study , 1993 .
[45] J. Holloway,et al. Water Sources for Subduction Zone Volcanism: New Experimental Constraints , 1993, Science.
[46] H. Mao,et al. Coesite-bearing eclogite from the Dabie Mountains in central China , 1989 .
[47] H. Roermund,et al. The pressure path of solid inclusions in minerals: the retention of coesite inclusions during uplift , 1986 .
[48] P. Gillet,et al. Coesite in subducted continental crust: P-T history deduced from an elastic model , 1984 .
[49] David C. Smith. Coesite in clinopyroxene in the Caledonides and its implications for geodynamics , 1984, Nature.
[50] C. Chopin. Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequences , 1984 .
[51] P. Wyllie,et al. Melting of Granite with Excess Water to 30 Kilobars Pressure , 1968, The Journal of Geology.
[52] E. Shoemaker,et al. First Natural Occurrence of Coesite , 1960, Science.
[53] L. Coes. A New Dense Crystalline Silica. , 1953, Science.