Melt segregation and magma interactions during crustal melting: Breaking out of the matrix

[1]  C. Fanning,et al.  The origin of extensive Neoarchean high-silica batholiths and the nature of intrusive complements to silicic ignimbrites: Insights from the Wyoming batholith, U.S.A. , 2016 .

[2]  R. Maas,et al.  Genesis of Felsic Plutonic Magmas and Their Igneous Enclaves: The Cobaw Batholith of Southeastern Australia , 2016, The Journal of Geology.

[3]  A. Glazner,et al.  Silicic Magmatism and the Volcanic–Plutonic Connection , 2016 .

[4]  M. Ducea,et al.  A MASH Zone Revealed: the Mafic Complex of the Sierra Valle Fértil , 2015 .

[5]  P. Lipman,et al.  Ignimbrites to batholiths: integrating perspectives from geological, geophysical, and geochronological data , 2015 .

[6]  J. Clemens Magmatic life at low Reynolds number: COMMENT , 2015 .

[7]  G. Nicoli,et al.  Rapid evolution from sediment to anatectic granulite in an Archean continental collision zone: the example of the Bandelierkop Formation metapelites, South Marginal Zone, Limpopo Belt, South Africa , 2015 .

[8]  G. N. Phillips,et al.  Inferring a deep-crustal source terrane from a high-level granitic pluton: the Strathbogie Batholith, Australia , 2014, Contributions to Mineralogy and Petrology.

[9]  A. Glazner Magmatic life at low Reynolds number , 2014 .

[10]  G. Stevens,et al.  Small-scale Hf isotopic variability in the Peninsula pluton (South Africa): the processes that control inheritance of source 176Hf/177Hf diversity in S-type granites , 2014, Contributions to Mineralogy and Petrology.

[11]  G. Nicoli,et al.  The processes that control leucosome compositions in metasedimentary granulites: perspectives from the Southern Marginal Zone migmatites, Limpopo Belt, South Africa , 2014 .

[12]  S. Lasalle,et al.  Anatectic record and contrasting P–T paths of aluminous gneisses from the central Grenville Province , 2014 .

[13]  G. Stevens,et al.  Extreme mineral-scale Sr isotope heterogeneity in granites by disequilibrium melting of the crust , 2014 .

[14]  R. Mills,et al.  Zircon U‐Pb geochronology of the Mount Givens Granodiorite: Implications for the genesis of large volumes of eruptible magma , 2014 .

[15]  M. Ducea,et al.  Petrogenetic Processes in a Deep Arc Section: A MASH Zone Revealed , 2013 .

[16]  M. Brown,et al.  Consequences of open-system melting in tectonics , 2013, Journal of the Geological Society.

[17]  J. Clemens Element concentrations in granitic magmas: ghosts of textures past? , 2013, Journal of the Geological Society.

[18]  R. Weinberg,et al.  Interaction between deformation and magma extraction in migmatites: Examples from Kangaroo Island, South Australia , 2013 .

[19]  C. Hawkesworth,et al.  Evidence for distinct stages of magma history recorded by the compositions of accessory apatite and zircon , 2013, Contributions to Mineralogy and Petrology.

[20]  A. Kisters,et al.  The stabilization of self-organised leucogranite networks—Implications for melt segregation and far-field melt transfer in the continental crust , 2012 .

[21]  M. Brown,et al.  Granite: From genesis to emplacement , 2012 .

[22]  R. Sparks,et al.  Melt Segregation in Deep Crustal Hot Zones: a Mechanism for Chemical Differentiation, Crustal Assimilation and the Formation of Evolved Magmas , 2012 .

[23]  G. Stevens,et al.  Multi-batch, incremental assembly of a dynamic magma chamber: the case of the Peninsula pluton granite (Cape Granite Suite, South Africa) , 2012, Mineralogy and Petrology.

[24]  I. Buick,et al.  Successive midcrustal, high-grade metamorphic events provide insight into Mid-Archean mountain-building along the SE margin of the proto-Kaapvaal craton , 2012 .

[25]  C. McLeod,et al.  Disequilibrium melting during crustal anatexis and implications for modeling open magmatic systems , 2012 .

[26]  G. Stevens,et al.  What controls chemical variation in granitic magmas , 2012 .

[27]  Anne M. Hofmeister,et al.  The influence of temperature-dependent thermal diffusivity on the conductive cooling rates of plutons and temperature-time paths in contact aureoles , 2012 .

[28]  I. Buick,et al.  Isotopic variations in S-type granites: an inheritance from a heterogeneous source? , 2012, Contributions to Mineralogy and Petrology.

[29]  G. Stevens,et al.  The enigmatic sources of I-type granites: The peritectic connexion , 2011 .

[30]  M. Brown,et al.  When the Continental Crust Melts , 2011 .

[31]  R. A. Dudley,et al.  Erratum to: S-type ignimbrites with polybaric crystallisation histories: the Tolmie Igneous Complex, Central Victoria, Australia , 2011 .

[32]  G. Stevens,et al.  Source controlled 87Sr/86Sr isotope variability in granitic magmas: The inevitable consequence of mineral-scale isotopic disequilibrium in the protolith , 2011 .

[33]  G. Stevens,et al.  Selective entrainment of peritectic garnet into S-type granitic magmas: Evidence from Archaean mid-crustal anatectites , 2010 .

[34]  M. Ghiorso,et al.  Rhyolite-MELTS: a Modified Calibration of MELTS Optimized for Silica-rich, Fluid-bearing Magmatic Systems , 2010 .

[35]  D. Okaya,et al.  Magmatic lobes as “snapshots” of magma chamber growth and evolution in large, composite batholiths: An example from the Tuolumne intrusion, Sierra Nevada, California , 2010 .

[36]  A. Harker,et al.  The Tertiary Igneous Rocks of Skye , 2010 .

[37]  I. Buick,et al.  Tracking S-type granite from source to emplacement: Clues from garnet in the Cape Granite Suite , 2009 .

[38]  A. Kisters,et al.  Melt segregation and far-field melt transfer in the mid-crust , 2009, Journal of the Geological Society.

[39]  M. Ducea,et al.  Generation of Tonalitic and Dioritic Magmas by Coupled Partial Melting of Gabbroic and Metasedimentary Rocks within the Deep Crust of the Famatinian Magmatic Arc, Argentina , 2009, Journal of Petrology.

[40]  I. Buick,et al.  The trace element compositions of S-type granites: evidence for disequilibrium melting and accessory phase entrainment in the source , 2009 .

[41]  G. Stevens,et al.  Chemical structure in granitic magmas – a signal from the source? , 2009, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[42]  G. Stevens,et al.  Fluid and deformation induced partial melting and melt volumes in low-temperature granulite-facies metasediments, Damara Belt, Namibia , 2008 .

[43]  J. Beard,et al.  Crystal–Melt Separation and the Development of Isotopic Heterogeneities in Hybrid Magmas , 2007 .

[44]  F. González-Lodeiro,et al.  Zircon Inheritance Reveals Exceptionally Fast Crustal Magma Generation Processes in Central Iberia during the Cambro-Ordovician , 2007 .

[45]  F. Costa,et al.  Equilibration Scales in Silicic to Intermediate Magmas—Implications for Experimental Studies , 2007 .

[46]  M. Brown,et al.  Crustal melting and melt extraction, ascent and emplacement in orogens: mechanisms and consequences , 2007, Journal of the Geological Society.

[47]  D. Perugini,et al.  Interplay between geochemistry and magma dynamics during magma interaction: An example from the Sithonia Plutonic Complex (NE Greece) , 2007 .

[48]  Colin J. N. Wilson,et al.  Compositional Zoning of the Bishop Tuff , 2007 .

[49]  Luca Valentini,et al.  The ‘small-world’ nature of fracture/conduit networks: Possible implications for disequilibrium transport of magmas beneath mid-ocean ridges , 2007 .

[50]  J. Vigneresse,et al.  Granitic batholiths: from pervasive and continuous melting in the lower crust to discontinuous and spaced plutonism in the upper crust , 2006, Transactions of the Royal Society of Edinburgh: Earth Sciences.

[51]  L. Font,et al.  Mineral-scale Sr isotope variation in plutonic rocks — a tool for unravelling the evolution of magma systems , 2006, Transactions of the Royal Society of Edinburgh: Earth Sciences.

[52]  A. Kisters,et al.  Progressive adjustments of ascent and emplacement controls during incremental construction of the 3.1 Ga Heerenveen batholith, South Africa , 2006 .

[53]  J. Clemens Melting of the continental crust: fluid regimes, melting reactions, and source-rock fertility , 2006 .

[54]  R. Sparks,et al.  The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot Zones , 2006 .

[55]  T. Wenzel,et al.  Sr isotope systematics of K-feldspars in plutonic rocks revealed by the Rb-Sr microdrilling technique , 2005 .

[56]  G. Poli,et al.  Microchemical and Sr Isotopic Investigation of Zoned K-feldspar Megacrysts: Insights into the Petrogenesis of a Granitic System and Disequilibrium Crystal Growth , 2005 .

[57]  M. Crawford,et al.  Reactive bulk assimilation: A model for crust-mantle mixing in silicic magmas , 2005 .

[58]  G. Stevens,et al.  Transcurrent shearing, granite sheeting and the incremental construction of the tabular 3.1 Ga Mpuluzi batholith, Barberton granite–greenstone terrane, South Africa , 2005, Journal of the Geological Society.

[59]  M. Handy,et al.  Experimental deformation of partially melted granite revisited: implications for the continental crust , 2005 .

[60]  J. Kalda,et al.  Melt extraction and accumulation from partially molten rocks , 2004 .

[61]  O. Bachmann,et al.  On the Origin of Crystal-poor Rhyolites: Extracted from Batholithic Crystal Mushes , 2004 .

[62]  A. Glazner,et al.  Rethinking the emplacement and evolution of zoned plutons: Geochronologic evidence for incremental assembly of the Tuolumne Intrusive Suite, California , 2004 .

[63]  M. Rabinowicz,et al.  Melt segregation under compaction and shear channeling: Application to granitic magma segregation in a continental crust , 2004 .

[64]  A. Glazner,et al.  Are plutons assembled over millions of years by amalgamation from small magma chambers , 2004 .

[65]  Calvin G. Barnes,et al.  Geology of a magma transfer zone: the Hortav沠Igneous Complex, north-central Norway , 2003 .

[66]  J. Richards Tectono-Magmatic Precursors for Porphyry Cu-(Mo-Au) Deposit Formation , 2003 .

[67]  D. Kohlstedt,et al.  Stress‐driven melt segregation in partially molten rocks , 2003 .

[68]  N. Petford,et al.  Source-Related Chemical and Isotopic Heterogeneities in Granitoids , 2003 .

[69]  J. Clemens S-type granitic magmas—petrogenetic issues, models and evidence , 2003 .

[70]  E. Sawyer,et al.  Large‐scale melt‐depletion in granulite terranes: an example from the Archean Ashuanipi Subprovince of Quebec , 2003 .

[71]  R. Powell,et al.  Melt loss and the preservation of granulite facies mineral assemblages , 2002 .

[72]  J. Davidson,et al.  Insights into Collisional Magmatism from Isotopic Fingerprints of Melting Reactions , 2002, Science.

[73]  C. Holyoke,et al.  An experimental study of grain scale melt segregation mechanisms in two common crustal rock types , 2002 .

[74]  T. Rushmer Volume change during partial melting reactions: implications for melt extraction, melt geochemistry and crustal rheology , 2001 .

[75]  B. Chappell,et al.  Two contrasting granite types: 25 years later , 2001 .

[76]  O. Vanderhaeghe Melt segragation, pervasive melt migration and magma mobility in the continental crust: the structural record from pores to orogens , 2001 .

[77]  A. Simakin,et al.  Transfer of melt between microscopic pores and macroscopic veins in migmatites , 2001 .

[78]  M. Brown,et al.  Crustal melting and granite magmatism: key issues , 2001 .

[79]  L. Kriegsman,et al.  Partial melting in crustal xenoliths and anatectic migmatites: a comparison , 2001 .

[80]  B. Evans,et al.  On the rheologically critical melt fraction , 2000 .

[81]  I. Nicholls,et al.  Fingerprinting feldspar phenocrysts using crystal isotopic composition stratigraphy: implications for crystal transfer and magma mingling in S-type granites , 2000 .

[82]  Uttam K. Bhui,et al.  Ultra-high Temperature Metamorphism of Metapelitic Granulites from Kondapalle, Eastern Ghats Belt: Implications for the Indo-Antarctic Correlation , 1999 .

[83]  E. Watson,et al.  Low melt fraction connectivity of granitic and tonalitic melts in a mafic crustal rock at 800 °C and 1 GPa , 1999 .

[84]  W. Duffield,et al.  A model that helps explain Sr-isotope disequilibrium between feldspar phenocrysts and melt in large-volume silicic magma systems , 1998 .

[85]  G. Droop,et al.  Fluids, P-T paths and the fates of anatectic melts in the Earth's crust , 1998 .

[86]  J. Clemens Observations on the origins and ascent mechanisms of granitic magmas , 1998, Journal of the Geological Society.

[87]  N. Petford,et al.  Self-organisation and fracture connectivity in rapidly heated continental crust , 1998 .

[88]  S. Harley Ultrahigh temperature granulite metamorphism (1050 °C, 12 kbar) and decompression in garnet (Mg70)–orthopyroxene–sillimanite gneisses from the Rauer Group, East Antarctica , 1998 .

[89]  G. Stevens,et al.  Melt production during granulite-facies anatexis: experimental data from “primitive” metasedimentary protoliths , 1997 .

[90]  J. Montel,et al.  Partial melting of metagreywackes, Part II. Compositions of minerals and melts , 1997 .

[91]  W. Collins,et al.  A three-component Sr-Nd isotopic mixing model for granitoid genesis, Lachlan fold belt, eastern Australia , 1997 .

[92]  P. Barbey,et al.  Rheological Transitions During Partial Melting and Crystallization with Application to Felsic Magma Segregation and Transfer , 1996 .

[93]  J. Pearce Sources and settings of granitic rocks , 1996 .

[94]  R. D'lemos Mixing between granitic and dioritic crystal mushes, Guernsey, Channel Islands, UK , 1996 .

[95]  B. Chappell Magma mixing and the production of compositional variation within granite suites: Evidence from the granites of southeastern Australia , 1996 .

[96]  Eugene I. Smith,et al.  Isotopic Disequilibrium among Commingled Hybrid Magmas: Evidence for a Two-Stage Magma Mixing-Commingling Process in the Mt. Perkins Pluton, Arizona , 1995, The Journal of Geology.

[97]  E. Watson,et al.  Experimental and theoretical constraints on melt distribution in crustal sources: the effect of crystalline anisotropy on melt interconnectivity , 1995 .

[98]  E. Mclellan,et al.  Melt segregation in migmatites , 1995 .

[99]  E. Rutter,et al.  Experimental deformation of partially molten Westerly granite under fluid‐absent conditions, with implications for the extraction of granitic magmas , 1995 .

[100]  T. Rushmer An experimental deformation study of partially molten amphibolite: Application to low‐melt fraction segregation , 1995 .

[101]  Kelsey A. Jordahl,et al.  Experiments on flow focusing in soluble porous media, with applications to melt extraction from the mantle , 1995 .

[102]  D. Laporte Wetting behavior of partial melts during crustal anatexis: the distribution of hydrous silicic melts in polycrystalline aggregates of quartz , 1994 .

[103]  M. Brown,et al.  The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustally-derived granite connection in thickened orogens , 1994 .

[104]  R. C. Kerr,et al.  Dike transport of granitoid magmas , 1993 .

[105]  E. Watson,et al.  A study of strontium diffusion in K-feldspar, Na-K feldspar and anorthite using Rutherford Backscattering Spectroscopy , 1992 .

[106]  J. Clemens,et al.  Granitic magma transport by fracture propagation , 1992 .

[107]  G. Stevens,et al.  Partial melting and the origin of metapelitic granulites in the Southern Marginal Zone of the Limpopo Belt, South Africa , 1992 .

[108]  I. Moreno-Ventas,et al.  H-type (hybrid) granitoids: a proposed revision of the granite-type classification and nomenclature , 1991 .

[109]  P. Wyllie,et al.  Dehydration-melting of solid amphibolite at 10 kbar: Textural development, liquid interconnectivity and applications to the segregation of magmas , 1991 .

[110]  B. Barbarin Plagioclase xenocrysts and mafic magmatic enclaves in some granitoids of the Sierra Nevada Batholith, California , 1990 .

[111]  J. Fountain,et al.  Melt segregation in anatectic granites: a thermo-mechanical model , 1989 .

[112]  J. Clemens Volume and composition relationships between granites and their lower crustal source regions: An example from central Victoria, Australia , 1988 .

[113]  J. Tullis,et al.  Experimental deformation of partially melted granitic aggregates , 1988 .

[114]  W. Hildreth,et al.  Crustal contributions to arc magmatism in the Andes of Central Chile , 1988 .

[115]  P. Wyllie,et al.  Interaction of granitic and basic magmas: experimental observations on contamination processes at 10 kbar with H2O , 1988 .

[116]  S. Wickham The segregation and emplacement of granitic magmas , 1987, Journal of the Geological Society.

[117]  B. Chappell,et al.  Comment and Reply on “S-type granites and their probable absence in southwestern North America” , 1986 .

[118]  R. Sparks,et al.  Thermal and mechanical constraints on mixing between mafic and silicic magmas , 1986 .

[119]  Nikolaus von Bargen,et al.  Permeabilities, interfacial areas and curvatures of partially molten systems: Results of numerical computations of equilibrium microstructures , 1986 .

[120]  B. Chappell,et al.  S-type granites and their probable absence in southwestern North America , 1986 .

[121]  D. McKenzie The extraction of magma from the crust and mantle , 1985 .

[122]  E. Watson,et al.  The distribution of partial melt in a granitic system: The application of liquid phase sintering theory , 1985 .

[123]  J. Whalen,et al.  The Topsails igneous terrane, Western Newfoundland: evidence for magma mixing , 1984 .

[124]  D. McKenzie,et al.  The Generation and Compaction of Partially Molten Rock , 1984 .

[125]  K. L. Cameron Bishop Tuff Revisited: New Rare Earth Element Data Consistent with Crystal Fractionation , 1984, Science.

[126]  P. Michael Chemical differentiation of the Bishop Tuff and other high-silica magmas through crystallization processes , 1983 .

[127]  D. DePaolo Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization , 1981 .

[128]  V. Wall,et al.  Origin and crystallization of some peraluminous (S-type) granitic magmas , 1981 .

[129]  G. Wasserburg,et al.  Petrogenetic mixing models and Nd-Sr isotopic patterns , 1979 .

[130]  A. Arzi Critical phenomena in the rheology of partially melted rocks , 1978 .

[131]  J. Weertman Theory of water-filled crevasses in glaciers applied to vertical magma transport beneath oceanic ridges , 1971 .

[132]  J. Moyen,et al.  Selective peritectic garnet entrainment as the origin of geochemical diversity in S-type granites , 2007 .

[133]  P. Nabelek,et al.  Fertility of metapelites and metagraywackes during leucogranite generation: an example from the Black Hills, U.S.A. , 2000, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[134]  N. Petford,et al.  Application of Information Theory to the Formation of Granitic Rocks , 1997 .

[135]  F. Bea Controls on the trace element composition of crustal melts , 1996, Earth and environmental science transactions of the Royal Society of Edinburgh.

[136]  E. Watson,et al.  Dissolution, growth and survival of zircons during crustal fusion: kinetic principals, geological models and implications for isotopic inheritance , 1996, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[137]  Peter J. Ortoleva,et al.  Geochemical Self-Organization , 1994 .

[138]  D. DePaolo,et al.  Crustal versus mantle sources of granitic magmas: a two-parameter model based on Nd isotopic studies , 1992, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[139]  C. Pin,et al.  Granites, Granulites, and Crustal Differentiation , 1990 .

[140]  W. Collins,et al.  Local, mid-crustal granulite facies metamorphism and melting: an example in the Mount Stafford area, central Australia , 1990 .

[141]  E. Watson,et al.  Perspectives on the source, segregation and transport of granitoid magmas , 1988, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[142]  J. Clemens Water contents of silicic to intermediate magmas , 1984 .

[143]  W. Hildreth The Bishop Tuff: Evidence for the origin of compositional zonation in silicic magma chambers , 1979 .