Formation of atoll garnets in the UHP eclogites of the Tso Morari Complex, Ladakh, Himalaya
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[1] B. Kaus,et al. Subduction metamorphism in the Himalayan ultrahigh-pressure Tso Morari massif: An integrated geodynamic and petrological modelling approach , 2017 .
[2] S. Thomas. Water in the Earth's Mantle: Mineral-specific IR Absorption Coefficients and Radiative Thermal Conductivities , 2015 .
[3] P. O'Brien,et al. Subduction, peak and multi-stage exhumation metamorphism: Traces from one coesite-bearing eclogite, Tso Morari, western Himalaya , 2015 .
[4] N. Chatterjee,et al. Exhumation of the UHP Tso Morari eclogite as a diapir rising through the mantle wedge , 2015, Contributions to Mineralogy and Petrology.
[5] K. Harvey. PRESSURE-TEMPERATURE-TIME CONSTRAINTS FOR UHP TSO MORARI ECLOGITE, NW INDIA , 2014 .
[6] M. Searle,et al. Phase equilibria modelling of retrograde amphibole and clinozoisite in mafic eclogite from the Tso Morari massif, northwest India: constraining the P–T–M(H2O) conditions of exhumation , 2014 .
[7] A. Webb,et al. Petrochronology of Himalayan ultrahigh-pressure eclogite , 2013 .
[8] N. Pant,et al. Insights into the P–T evolution path of Tso Morari eclogites of the north-western Himalayas: Constraints on the geodynamic evolution of the region , 2013, Journal of Earth System Science.
[9] M. Searle,et al. Integrated pressure–temperature–time constraints for the Tso Morari dome (Northwest India): implications for the burial and exhumation path of UHP units in the western Himalaya , 2013 .
[10] A. Pêcher,et al. Deciphering high-pressure metamorphism in collisional context using microprobe mapping methods: Application to the Stak eclogitic massif (northwest Himalaya) , 2013 .
[11] K. Mulchrone,et al. Estimating the viscosity and Prandtl number of the Tso Morari crystalline gneiss dome, Indian western Himalaya , 2012, International Journal of Earth Sciences.
[12] M. D. R. Cruz. Origin of atoll garnet in schists from the Alpujárride Complex (Central zone of the Betic Cordillera, Spain): Implications on the P-T evolution , 2011 .
[13] P. O'Brien,et al. The multistage exhumation history of the Kaghan Valley UHP series, NW Himalaya, Pakistan from U-Pb and 40Ar/39Ar ages , 2010 .
[14] H. Klápová,et al. Mechanism of formation of atoll garnet during high-pressure metamorphism , 2010, Mineralogical Magazine.
[15] B. K. Mukherjee,et al. Fluids in coesite-bearing rocks of the Tso Morari Complex, NW Himalaya: evidence for entrapment during peak metamorphism and subsequent uplift , 2009, Geological Magazine.
[16] P. O'Brien,et al. Garnet growth at high- and ultra-high pressure conditions and the effect of element fractionation on mineral modes and composition , 2008 .
[17] A. Pêcher,et al. Tethyan and Indian subduction viewed from the Himalayan high- to ultrahigh-pressure metamorphic rocks , 2008 .
[18] J. Epard,et al. Structural development of the Tso Morari ultra-high pressure nappe of the Ladakh Himalaya , 2008 .
[19] P. O'Brien,et al. Compositional re-equilibration of garnet: the importance of sub-grain boundaries , 2007 .
[20] K. Kobayashi,et al. Origin of atoll garnets in eclogites and implications for the redistribution of trace elements during slab exhumation in a continental subduction zone , 2007 .
[21] E. Havrns. Fluid-assisted modification of garnet composition along rims , cracks , and mineral inclusion boundaries in samples of amphibolite facies schists , 2007 .
[22] M. Searle,et al. Plate velocity exhumation of ultrahigh-pressure eclogites in the Pakistan Himalaya , 2006 .
[23] M. Bickle,et al. Contrasting depth-temperature-time histories of the High and Lesser Himalaya of NW India , 2006 .
[24] N. Bolfan-Casanova. Water in the Earth’s mantle , 2005, Mineralogical Magazine.
[25] S. Klemperer,et al. The onset of India-Asia continental collision: Early, steep subduction required by the timing of UHP metamorphism in the western Himalaya [rapid communication] , 2005 .
[26] S. Poli,et al. Experimentally Determined Phase Relations in Hydrous Peridotites to 6·5 GPa and their Consequences on the Dynamics of Subduction Zones , 2004 .
[27] Yong‐Fei Zheng,et al. Low-T eclogite in the Dabie terrane of China: petrological and isotopic constraints on fluid activity and radiometric dating , 2004 .
[28] K. Pogue,et al. Tectonostratigraphic subdivisions of the Himalaya: A view from the west , 2004 .
[29] H. Keppler,et al. The temperature dependence of water solubility in enstatite , 2004 .
[30] E. Ravna,et al. Geothermobarometry of UHP and HP eclogites and schists – an evaluation of equilibria among garnet–clinopyroxene–kyanite–phengite–coesite/quartz , 2004 .
[31] C. Robert-Charrue,et al. Folding and inversion tectonics in the Anti‐Atlas of Morocco , 2004 .
[32] G. Hoinkes,et al. Complex Growth Textures in a Polymetamorphic Metabasite from the Kraubath Massif (Eastern Alps) , 2004 .
[33] S. Guillot,et al. Exhumation of the ultrahigh‐pressure Tso Morari unit in eastern Ladakh (NW Himalaya): A case study , 2004 .
[34] S. Maruyama,et al. Discovery of coesite from Indus Suture Zone (ISZ), Ladakh, India: Evidence for deep subduction , 2004 .
[35] F. Keller,et al. The South Ladakh ophiolites (NW Himalaya, India): an intra-oceanic tholeiitic arc origin with implication for the closure of the Neo-Tethys , 2004 .
[36] M. Kohn. 3.07 – Geochemical Zoning in Metamorphic Minerals , 2003 .
[37] P. Shen,et al. On the mechanism of resorption zoning in metamorphic garnet , 2003 .
[38] I. Katayama,et al. Timing of Himalayan ultrahigh‐pressure metamorphism: sinking rate and subduction angle of the Indian continental crust beneath Asia , 2003 .
[39] F. Seno,et al. Unraveling the Schneeberg garnet puzzle: a numerical model of multiple nucleation and coalescence , 2003 .
[40] Yong‐Fei Zheng,et al. Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie–Sulu orogen in China: implications for geodynamics and fluid regime , 2003 .
[41] D. Baratoux,et al. Reconstructing the total shortening history of the NW Himalaya , 2003 .
[42] M. Cosca,et al. Exhumation history of eastern Ladakh revealed by 40Ar/39Ar and fission-track ages: the Indus River–Tso Morari transect, NW Himalaya , 2003, Journal of the Geological Society.
[43] B. K. Mukherjee,et al. Carbonate-Bearing UHPM Rocks from the Tso-Morari Region, Ladakh, India: Petrological Implications , 2003 .
[44] D. Prior,et al. An overgrowth model to explain multiple, dispersed high-Mn regions in the cores of garnet porphyroblasts , 2003 .
[45] K. Ye,et al. Cluster of water molecules in garnet from ultrahigh-pressure eclogite , 2002 .
[46] J. Miller,et al. Fluid processes during the exhumation of high-P metamorphic belts , 2002, Mineralogical Magazine.
[47] T. Nägler,et al. Evidence of hydration of the mantle wedge and its role in the exhumation of eclogites , 2001 .
[48] T. Harrison,et al. Cenozoic structural and metamorphic evolution of the eastern Himalayan syntaxis (Namche Barwa) , 2001 .
[49] D. Prior,et al. Development of garnet porphyroblasts by multiple nucleation, coalescence and boundary misorientation-driven rotations , 2001 .
[50] P. O'Brien,et al. Coesite in Himalayan eclogite and implications for models of India-Asia collision , 2001 .
[51] J. Hoefs,et al. Geochemical constraints of the eclogite and granulite facies metamorphism as recognized in the Raobazhai complex from North Dabie Shan, China , 2001 .
[52] B. K. Mukherjee,et al. Discovery of coesite from Indian Himalaya: A record of ultra-high pressure metamorphism in Indian Continental Crust , 2001 .
[53] M. Kohn,et al. Retrograde net transfer reaction insurance for pressure-temperature estimates , 2000 .
[54] J. Mosenfelder. Pressure dependence of hydroxyl solubility in coesite , 2000 .
[55] J. Blichert‐Toft,et al. Dating the Indian continental subduction and collisional thickening in the northwest Himalaya: Multichronology of the Tso Morari eclogites , 2000 .
[56] J. Hoefs,et al. Fluid history of UHP metamorphism in Dabie Shan, China: a fluid inclusion and oxygen isotope study on the coesite-bearing eclogite from Bixiling , 2000 .
[57] H. Skogby,et al. Hydrogen in nominally anhydrous upper-mantle minerals: concentration levels and implications;Hydrogen in nominally anhydrous upper-mantle minerals: concentration levels and implications , 2000 .
[58] H. Skogby,et al. Hydrogen in nominally anhydrous upper-mantle minerals concentration levels and implications , 2000 .
[59] Krogh Ravna. The garnet–clinopyroxene Fe2+–Mg geothermometer: an updated calibration , 2000 .
[60] M. Fialin,et al. Rates of thermal equilibration at the onset of subduction deduced from diffusion modeling of eclogitic garnets, Yukon-Tanana terrane, Canada , 1999 .
[61] Yong‐Fei Zheng,et al. Hydrogen and oxygen isotope evidence for fluid–rock interactions in the stages of pre- and post-UHP metamorphism in the Dabie Mountains , 1999 .
[62] C. Szabó,et al. Exhumation History of Eclogites from the Tso-Morari Crystalline Complex in Eastern Ladakh: Mineralogical and Fluid Inclusion Constraints , 1999 .
[63] S. Poli,et al. Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation , 1998 .
[64] B. Wood,et al. THE OH CONTENT OF PYROPE AT HIGH PRESSURE , 1998 .
[65] J. Epard,et al. Geological transect across the Tso Morari and Spiti areas: The nappe structures of the Tethys Himalaya , 1998 .
[66] R. Trumbull,et al. On Li-Bearing Micas: Estimating Li from Electron Microprobe Analyses and an Improved Diagram for Graphical Representation , 1997, Mineralogical Magazine.
[67] H. Keppler,et al. Water solubility in pyrope to 100 kbar , 1997 .
[68] S. Guillot,et al. Glaucophane-bearing eclogites in the Tso Morari dome (eastern Ladakh, NW Himalaya) , 1997 .
[69] S. Guillot,et al. Eclogitic metasediments from the Tso Morari area (Ladakh, Himalaya): evidence for continental subduction during India-Asia convergence , 1997 .
[70] S. Poli,et al. The high-pressure stability of hydrous phases in orogenic belts: an experimental approach on eclogite-forming processes , 1997 .
[71] G. Rossman. Studies of OH in nominally anhydrous minerals , 1996 .
[72] D. Whitney. Garnets as open systems during regional metamorphism , 1996 .
[73] S. Poli,et al. H2O transport and release in subduction zones : experimental constraints on basaltic and andesitic systems , 1995 .
[74] S. Tonarini,et al. Geochemical and Sr-Nd isotopic characterisation of higher Himalayan eclogites (and associated metabasites) , 1995 .
[75] F. Spear,et al. Metamorphism of Calcic Pelitic Schists, Strafford Dome, Vermont: Compositional Zoning and Reaction History , 1993 .
[76] S. Peacock. The importance of blueschist → eclogite dehydration reactions in subducting oceanic crust , 1993 .
[77] Thomas Menard,et al. FLUID-ASSISTED MODIFICATION OF GARNET COMPOSITION ALONG RIMS, CRACKS, AND MINERAL INCLUSION BOUNDARIES IN SAMPLES OF AMPHIBOLITE FACIES SCHISTS , 1993 .
[78] D. Waters. Geobarometry of phengite-bearing eclogites , 1993 .
[79] A. Thompson. Water in the Earth's upper mantle , 1992, Nature.
[80] G. Rossman,et al. Water in Earth's Mantle: The Role of Nominally Anhydrous Minerals , 1992, Science.
[81] G. Rossman,et al. Incorporation of hydroxyl in upper-mantle clinopyroxenes , 1991, Nature.
[82] F. Spear,et al. Effects of diffusional modification of garnet growth zoning on P-T path calculations , 1991 .
[83] D. Whitney. Calcium depletion halos and Fe-Mn-Mg zoning around faceted plagioclase inclusions in garnet from a high-grade pelitic gneiss , 1991 .
[84] R. Joesten. Grain-Boundary Diffusion Kinetics in Silicate and Oxide Minerals , 1991 .
[85] B. W. Evans. Phase relations of epidote-blueschists , 1990 .
[86] D. A. Carswell. Eclogites and the eclogite facies; definitions and classification , 1990 .
[87] R. Oberhänsli,et al. Eclogite facies mineral parageneses , 1990 .
[88] Roger Powell,et al. An enlarged and updated internally consistent thermodynamic dataset with uncertainties and correlations: the system K2O–Na2O–CaO–MgO–MnO–FeO–Fe2O3–Al2O3–TiO2–SiO2–C–H2–O2 , 1990 .
[89] R. C. Newton,et al. Reversed experimental calibration of the garnet-clinopyroxene Fe — Mg exchange thermometer , 1989 .
[90] Nobuo Morimoto,et al. Nomenclature of Pyroxenes , 1988, Mineralogical Magazine.
[91] E. J. Krogh. The garnet-clinopyroxene Fe-Mg geothermometer — a reinterpretation of existing experimental data , 1988 .
[92] F. Spear,et al. Trace-element zoning in a metamorphic garnet , 1987 .
[93] J. Ridley. Evidence of a Temperature-dependent ‘Blueschist’ to ‘Eclogite’ Transformation in High-pressure Metamorphism of Metabasic Rocks , 1984 .
[94] P. Gillet,et al. Coesite in subducted continental crust: P-T history deduced from an elastic model , 1984 .
[95] David C. Smith. Coesite in clinopyroxene in the Caledonides and its implications for geodynamics , 1984, Nature.
[96] C. Chopin. Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequences , 1984 .
[97] F. Spear,et al. Quantitative P-T paths from zoned minerals: Theory and tectonic applications , 1983 .
[98] T. Holland. The experimental determination of activities in disordered and short-range ordered jadeitic pyroxenes , 1983 .
[99] A. Lasaga. Geospeedometry: An Extension of Geothermometry , 1983 .
[100] T. Green,et al. FeMg partitioning between coexisting garnet and phengite at high pressure, and comments on a garnet-phengite geothermometer , 1982 .
[101] Steven R. Bohlen,et al. The quartz ⇆ coesite transformation: A precise determination and the effects of other components , 1982 .
[102] L. Medaris. A tectonic mélange of foreign eclogites and ultramafites in West Norway , 1980, Nature.
[103] David C. Smith. A tectonic mélange of foreign eclogites and ultramafites in West Norway , 1980, Nature.
[104] W. Griffin,et al. Caledonian Sm–Nd ages and a crustal origin for Norwegian eclogites , 1980, Nature.
[105] T. Holland. The reaction albite = jadeite+quartz determined experimentally in the range 600-1200 degrees C , 1980 .
[106] D. Green,et al. An experimental study of the effect of Ca upon garnet-clinopyroxene Fe-Mg exchange equilibria , 1979 .
[107] D. Smith,et al. Mantle-equilibrated Orthopyroxene Eclogite Pods from the Basal Gneisses in the Selje District, Western Norway , 1978 .
[108] A. Lasaga,et al. The Mathematics of Cation Diffusion and Exchange Between Silicate Minerals During Retrograde Metamorphism , 1977 .
[109] T. Loomis. Reaction of zoning of garnet , 1975 .
[110] J. Smellie. Formation of atoll garnets from the aureole of the Ardara pluton, Co. Donegal, Ireland , 1974, Mineralogical Magazine.
[111] B. Leake,et al. Report. Nomenclature of Amphiboles: Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names , 1971, Mineralogical Magazine.
[112] F. Forestier,et al. Découverte de niveaux d'amphibolites à pargasite, anorthite, corindon et saphirine dans les schistes cristallins de la vallée du Haut-Allier , 1969 .
[113] Joseph V. Smith,et al. Investigations concerning the Breakdown of Albite at Depth in the Earth , 1967, The Journal of Geology.
[114] L. Hollister. Garnet Zoning: An Interpretation Based on the Rayleigh Fractionation Model , 1966, Science.
[115] R. Howie,et al. An Introduction to the Rock-Forming Minerals , 1966 .
[116] R. Coleman,et al. Eclogites and Eclogites: Their Differences and Similarities , 1965 .
[117] W. Williamson. The Composite Gneiss and Contaminated Granodiorite of Glen Shee, Perthshire , 1935, Quarterly Journal of the Geological Society of London.
[118] J. Green. The Garnets and Streaky Rocks of the English Lake District , 1915 .