Water solubility in coesite at realistic temperatures o8f subduction zones

[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.