The 10Å phase: a high-pressure expandable sheet silicate stable during subduction of hydrated lithosphere

[1]  D. Günther,et al.  High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions , 2001 .

[2]  Fumagalli Patrizia,et al.  Phase relationships in hydrous peridotites at high presssure: preliminary results of multianvil experiments , 1999 .

[3]  M. I. Bell,et al.  Raman spectra and vibrational analysis of the trioctahedral mica phlogopite , 1999 .

[4]  K. Okamoto,et al.  The high-pressure synthesis of lawsonite in the MORB+H2O system , 1999 .

[5]  S. Clark,et al.  In situ observation of the formation of 10 angstrom phase from talc plus H2O at mantle pressures and temperatures , 1999 .

[6]  S. Poli,et al.  Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation , 1998 .

[7]  T. Fockenberg An experimental study of the pressure-temperature stability of MgMgAl-pumpellyite in the system MgO-Al2O3-SiO2-H2O , 1998 .

[8]  W. Schreyer,et al.  Antigorite: High-pressure stability in the system MgOSiO2H2O (MSH) , 1997 .

[9]  H. T. Haselton,et al.  The hydrothermal diamond anvil cell (HDAC) and its applications , 1996 .

[10]  G. Rossman,et al.  FTIR spectroscopy of lawsonite between 82 and 325 K , 1996 .

[11]  H. Keppler Constraints from partitioning experiments on the composition of subduction-zone fluids , 1996, Nature.

[12]  Jianzhong Zhang,et al.  In situ X-ray observations of the coesite-stishovite transition: reversed phase boundary and kinetics , 1996 .

[13]  B. Wood,et al.  The high-pressure stability of talc and 10 Å phase: Potential storage sites for H2O in subduction zones , 1995 .

[14]  J. G. Liou,et al.  Significance of ultrahigh-P talc-bearing eclogitic assemblages , 1995, Mineralogical Magazine.

[15]  W. Schreyer,et al.  Metastability of the 10-Å Phase in the System MgO–SiO2–H2O (MSH). What about Hydrous MSH Phases in Subduction Zones? , 1992 .

[16]  M. Frey,et al.  A new petrogenetic grid for low‐grade metabasites , 1991 .

[17]  S. Guggenheim,et al.  The incorporation of "water" in a high-pressure 2:1 layer silicate; a high pressure differential thermal analysis of the 10 Aa phase , 1991 .

[18]  O. Shimomura,et al.  Garnet-perovskite transformation in CaGeO3: In-situ X-ray measurements using synchrotron radiation , 1985 .

[19]  G. Rossman,et al.  The high temperature behavior of water and carbon dioxide in cordierite and beryl , 1984 .

[20]  O. Medenbach,et al.  Kulkeite, a new metamorphic phyllosilicate mineral: Ordered 1∶1 chlorite/talc mixed-layer , 1982 .

[21]  C. Chopin Talc-Phengite: a Widespread Assemblage in High-Grade Pelitic Blueschists of the Western Alps , 1981 .

[22]  J. Bauer,et al.  The 10A phase in the system MgO-SiO 2 -H 2 O , 1981 .

[23]  G. J. Rosasco,et al.  Raman Microprobe Spectra and Vibrational Mode Assignments of Talc , 1980 .

[24]  D. Bish,et al.  The nature of kerolite, its relation to talc and stevensite , 1977, Mineralogical Magazine.

[25]  S. Akimoto,et al.  The system MgO-SiO 2 -H 2 O at high pressures and temperatures; stability field for hydroxyl-chondrodite, hydroxyl-clinohumite and 10 A o -phase , 1977 .

[26]  R. Wilkins,et al.  Spectroscopic study of oxonium ions in minerals , 1974 .

[27]  J. Sharp,et al.  Method of Comparing Solid‐State Kinetic Data and Its Application to the Decomposition of Kaolinite, Brucite, and BaCO3 , 1972 .

[28]  S. Shimoda Mineralogical studies of a species of stevensite from the Obori mine, Yamagata Prefecture, Japan , 1971, Clay Minerals.

[29]  D. L. Hamilton,et al.  The Preparation of Silicate Compositions by a Gelling Method , 1968 .

[30]  G. V. Yukhnevich ADVANCES IN THE USE OF INFRARED SPECTROSCOPY FOR THE CHARACTERISATION OF OH BONDS , 1963 .

[31]  J. White,et al.  Infrared Spectra of Hydronium Ion in Micaceous Minerals , 1963, Science.

[32]  K. Nakamoto,et al.  Stretching Frequencies as a Function of Distances in Hydrogen Bonds , 1955 .