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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
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Huelva Spain (1)
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Jaen Spain (1)
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Betic Cordillera (1)
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United States
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New Mexico
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Dona Ana County New Mexico
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Kilbourne Hole (1)
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commodities
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ceramic materials (1)
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graphite deposits (1)
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industrial minerals (1)
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elements, isotopes
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metals
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alkaline earth metals
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barium (1)
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calcium (1)
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copper (1)
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iron (1)
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lead (1)
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nickel (1)
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phosphorus (1)
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fossils
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Chordata
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Vertebrata
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Theria
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Invertebrata
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Cnidaria
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Anthozoa
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geologic age
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Jurassic (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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ultramafics
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peridotites
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spinel lherzolite (1)
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volcanic rocks
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basalts
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carbonates
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calcite (1)
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native elements
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phosphates
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apatite (4)
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silicates
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chain silicates
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pyroxene group
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clinopyroxene (1)
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sulfides (1)
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Primary terms
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ceramic materials (1)
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chemical analysis (1)
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia
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Theria
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Eutheria
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Cetacea (1)
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crystal chemistry (1)
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crystal structure (4)
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environmental geology (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
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Huelva Spain (1)
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Jaen Spain (1)
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Betic Cordillera (1)
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-
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-
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graphite deposits (1)
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igneous rocks
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plutonic rocks
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ultramafics
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peridotites
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spinel lherzolite (1)
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volcanic rocks
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basalts
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alkali basalts (1)
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inclusions
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fluid inclusions (1)
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industrial minerals (1)
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Invertebrata
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Cnidaria
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Anthozoa
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Zoantharia
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Scleractinia
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Porites (1)
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Mollusca (1)
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mantle (1)
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Mesozoic
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Jurassic (1)
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metals
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alkaline earth metals
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barium (1)
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calcium (1)
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copper (1)
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iron (1)
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lead (1)
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nickel (1)
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mineral deposits, genesis (1)
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petrology (1)
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phosphorus (1)
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pollution (1)
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spectroscopy (2)
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United States
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New Mexico
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Dona Ana County New Mexico
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Kilbourne Hole (1)
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waste disposal (1)
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Welcome to Raman Spectroscopy: Successes, Challenges, and Pitfalls
Geoscience Meets Biology: Raman Spectroscopy in Geobiology and Biomineralization
A Technological Gem: Materials, Medical, and Environmental Mineralogy of Apatite
A-type substitution in carbonated strontium fluor-, chlor- and hydroxylapatites
Structural effects on incorporated water in carbonated apatites
Synthesis and structure of carbonated barium and lead fluorapatites: Effect of cation size on A-type carbonate substitution
Chemistry of bone mineral, based on the hypermineralized rostrum of the beaked whale Mesoplodon densirostris
Bone and Tooth Mineralization: Why Apatite?
Vein-type graphite in Jurassic volcanic rocks of the external zone of the Betic Cordillera, southern Spain
Interpretation of the sulfide assemblages in a suite of xenoliths from Kilbourne Hole, New Mexico
Petrography and electron microprobe analysis were used to investigate the mineralogy, bulk composition, abundance, and distribution of Cu-Fe-Ni sulfide phases in a suite of about 25 alkalic-basalt-hosted xenoliths from Kilbourne Hole, New Mexico. The xenoliths include spinel lherzolites, spinel clinopyroxenites, clinopyroxene megacrysts, mafic granuloblastites, and a sillimanite-quartz granuloblastite. Sulfide abundance is low in all the xenoliths, but shows a maximum (∼0.5 vol. %) in pyroxenites and megacrysts. The sulfides occur as interstitial to silicate and oxide grains, fully enclosed and isolated in grains, and along fracture surfaces in grains. The major sulfide phase is monosulfide solid solution (∼pyrrhotite), accompanied by variable amounts of pentlandite, and cubanite. Both the mineralogy and bulk sulfide composition are distinguishable among the xenolith types: Ni-rich for the lherzolites, Ni-poor for the crustal xenoliths, and intermediate for the pyroxenites, megacrysts, and composite xenoliths. The sulfides in the Kilbourne Hole spinel lherzolites most likely result from partial retention, in the residual silicate rock, of an immiscible sulfide formed during mantle partial melting.