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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Primary terms
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Meguma Terrane (1)
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carbon
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Cenozoic
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Quaternary (1)
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Tertiary
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Neogene
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Miocene
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upper Miocene
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Paleogene
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porphyry (2)
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inclusions
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isotopes
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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stable isotopes
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D/H (2)
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deuterium (1)
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Nd-144/Nd-143 (1)
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O-18/O-16 (2)
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Pb-206/Pb-204 (1)
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Triassic
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Mole Granite (1)
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metal ores
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copper ores (5)
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gold ores (6)
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lead ores (2)
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lead-zinc deposits (2)
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niobium ores (1)
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polymetallic ores (1)
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silver ores (3)
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tin ores (1)
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uranium ores (1)
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zinc ores (2)
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metals
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Sr-87/Sr-86 (2)
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copper (1)
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gold (1)
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iron (1)
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lead
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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Oceania
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orogeny (2)
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oxygen
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North Pacific
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Northeast Pacific
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Blanco fracture zone (1)
-
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-
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Paleozoic
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Carboniferous
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Mississippian
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Barnett Shale (1)
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Upper Pennsylvanian (1)
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Devonian
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Gile Mountain Formation (1)
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paragenesis (6)
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Precambrian
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Great Smoky Group (1)
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upper Precambrian
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Proterozoic
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Paleoproterozoic
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Qinling Group (1)
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sea water (1)
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sedimentary rocks
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limestone (1)
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chemically precipitated rocks
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clastic rocks
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Piceance Basin (1)
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Connecticut
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Litchfield County Connecticut (1)
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Delaware Basin (1)
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Hawaii
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Hawaii County Hawaii
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Hawaii Island
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Kilauea (2)
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Illinois
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Mojave Desert (1)
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Eureka County Nevada (1)
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New England (1)
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Oregon (1)
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Polk County Tennessee
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Texas
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Fort Worth Basin (1)
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chemically precipitated rocks
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clastic rocks
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-
Opening-mode fracturing and cementation during hydrocarbon generation in shale: An example from the Barnett Shale, Delaware Basin, West Texas
Formation of miarolitic-class, segregation-type pegmatites in the Taishanmiao batholith, China: The role of pressure fluctuations and volatile exsolution during pegmatite formation in a closed, isochoric system
Characterization of the metasomatizing agent in the upper mantle beneath the northern Pannonian Basin based on Raman imaging, FIB-SEM, and LA-ICP-MS analyses of silicate melt inclusions in spinel peridotite
Evaluation and application of the quartz-inclusions-in-epidote mineral barometer
Microscale Chemistry: Raman Analysis of Fluid and Melt Inclusions
Natrocarbonatites: A hidden product of three-phase immiscibility
A pedagogical approach to estimating the CO 2 budget of magmas
How Precisely Can the Temperature of a Fluid Event be Constrained Using Fluid Inclusions?
Upper mantle origin of plagioclase megacrysts from plagioclase-ultraphyric mid-oceanic ridge basalt
ABSTRACT Much of the early prograde history in metamorphic rocks is lost due to overprinting at near-peak conditions or through retrograde modification during exhumation. Fortunately, inclusions encapsulated in rigid porphyroblasts may preserve a record of early burial conditions. Quartz inclusions in garnet porphyroblasts from the Strafford Dome, eastern Vermont, have homogeneous Ti concentrations ([Ti]) that differ from matrix quartz, which retains a history of Si-liberating metamorphic reactions and fluid influx. We applied growth-composition models to evaluate potential processes associated with Ti partitioning in quartz before encapsulation in garnet, including a model for constant-volume growth of quartz due to mineral dissolution-transfer processes and growth as a result of Si-liberating diagenetic and metamorphic reactions. Because these processes typically occur at low temperatures, quartz with exceedingly low [Ti] (<<1 ppm) would be formed and cannot account for the homogeneous Ti distribution at concentrations between 2.5 and 5 ppm observed in the sample. This suggests that chemical reequilibration through dynamic recrystallization must have taken place prior to encapsulation in garnet. Analysis of fluid and graphite inclusions with Raman spectroscopy in different microstructural settings allowed the characterization of fluid composition and temperature of microstructure development early in the prograde history. The findings from this study exemplify the utility of garnet hosts to shield inclusion minerals from chemical modification and recrystallization during later events. As such, they provide a window into the early stages of orogenesis and provide insights concerning the mechanisms controlling equilibration of quartz.