about
Messengers from the deep: Fossil wadsleyite-chromite microstructures from the Mantle Transition ZoneContinental crust beneath southeast IcelandExtreme lithium isotopic fractionation in three zircon standards (Plešovice, Qinghu and Temora).Plume-subduction interaction forms large auriferous provinces.In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle.Synthesis of inverse ringwoodite sheds light on the subduction history of Tibetan ophiolites.Ultradeep continental roots and their oceanic remnants: A solution to the geochemical “mantle reservoir” problem?Fluid-present deformation aids chemical modification of chromite: Insights from chromites from Golyamo Kamenyane, SE BulgariaPink color in Type I diamonds: Is deformation twinning the cause?Raw material sources and an exchange network of the earliest farming society in central SwedenUse and misuse of Mg- and Mn-rich ilmenite in diamond exploration: A petrographic and trace element approachTrace-element geochemistry and U–Pb dating of perovskite in kimberlites of the Lunda Norte province (NE Angola): Petrogenetic and tectonic implicationsComposition of diamond-forming media in cuboid diamonds from the V. Grib kimberlite pipe (Arkhangelsk province, Russia)Recurrent magmatic activity on a lithosphere-scale structure: Crystallization and deformation in kimberlitic zirconsVolatile-bearing minerals and lithophile trace elements in the upper mantleTitanates of the lindsleyite–mathiasite (LIMA) group reveal isotope disequilibrium associated with metasomatism in the mantle beneath Kimberley (South Africa)The final stages of kimberlite petrogenesis: Petrography, mineral chemistry, melt inclusions and Sr-C-O isotope geochemistry of the Bultfontein kimberlite (Kimberley, South Africa)Sulfur isotope composition of metasomatised mantle xenoliths from the Bultfontein kimberlite (Kimberley, South Africa): Contribution from subducted sediments and the effect of sulfide alteration on S isotope systematicsChemical abrasion of zircon and ilmenite megacrysts in the Monastery kimberlite: Implications for the composition of kimberlite meltsZircon recycling and crystallization during formation of chromite- and Ni-arsenide ores in the subcontinental lithospheric mantle (Serranía de Ronda, Spain)The architecture of the European-Mediterranean lithosphere: A synthesis of the Re-Os evidenceTransfer of Os isotopic signatures from peridotite to chromitite in the subcontinental mantle: Insights from in situ analysis of platinum-group and base-metal minerals (Ojén peridotite massif, southern Spain)In situ Re–Os isotopic analysis of platinum-group minerals from the Mayarí-Cristal ophiolitic massif (Mayarí-Baracoa Ophiolitic Belt, eastern Cuba): implications for the origin of Os-isotope heterogeneities in podiform chromititesPersistence of mantle lithospheric Re–Os signature during asthenospherization of the subcontinental lithospheric mantle: insights from in situ isotopic analysis of sulfides from the Ronda peridotite (Southern Spain)Trace-element zonation in garnets from The Thumb: heating and melt infiltration below the Colorado PlateauGarnet geotherms: Pressure-temperature data from Cr-pyrope garnet xenocrysts in volcanic rocksIn situ U–Pb Dating and Sr–Nd Isotopic Analysis of Perovskite: Constraints on the Age and Petrogenesis of the Kuruman Kimberlite Province, Kaapvaal Craton, South AfricaNeoproterozoic magmatic flare-up along the N. margin of Gondwana: The Taknar complex, NE IranCrustal Evolution of NW Iran: Cadomian Arcs, Archean Fragments and the Cenozoic Magmatic Flare-UpMagmatic evolution of the ultramafic–mafic Kharaelakh intrusion (Siberian Craton, Russia): insights from trace-element, U–Pb and Hf-isotope data on zirconGZ7 and GZ8 - Two Zircon Reference Materials for SIMS U-Pb Geochronology.Microinclusions in monocrystalline octahedral diamonds and coated diamonds from Diavik, Slave Craton: Clues to diamond genesisSulfide and whole rock Re–Os systematics of eclogite and pyroxenite xenoliths from the Slave Craton, CanadaInsights into the mantle geochemistry of scandium from a meta-analysis of garnet dataCompositional effects on the solubility of minor and trace elements in oxide spinel minerals: Insights from crystal-crystal partition coefficients in chromite exsolutionThermal metamorphism of mantle chromites and the stability of noble-metal nanoparticlesChromitites in ophiolites: How, where, when, why? Part I. A review and new ideas on the origin and significance of platinum-group mineralsChromitites in ophiolites: How, where, when, why? Part II. The crystallization of chromititesCorrigendum to “Chromitites in ophiolites: How, where, when, why? Part II. The crystallisation of chromitites”Deposits associated with ultramafic–mafic complexes in Mexico: the Loma Baya case
P50
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P50
description
hulumtues
@sq
onderzoeker
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researcher
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հետազոտող
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name
William L. Griffin
@ast
William L. Griffin
@en
William L. Griffin
@es
William L. Griffin
@nl
William L. Griffin
@sl
type
label
William L. Griffin
@ast
William L. Griffin
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William L. Griffin
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William L. Griffin
@nl
William L. Griffin
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Griffin W L
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William L Griffin
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prefLabel
William L. Griffin
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William L. Griffin
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William L. Griffin
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William L. Griffin
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William L. Griffin
@sl
P1053
F-7713-2011
P106
P1153
35229299300
57200601013
P21
P31
P3829
P496
0000-0002-0980-2566