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The Canadian Mineralogist, 2002
To date, the evaluation of the temperature ( T) and pressure (P) of formation of natural diamond has generally relied on thermobarometry of rare polymineralic inclusions containing appropriate assemblages of minerals. The results are commonly ambiguous, because of potential re-equilibration of touching minerals after diamond growth and possible ...
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To date, the evaluation of the temperature ( T) and pressure (P) of formation of natural diamond has generally relied on thermobarometry of rare polymineralic inclusions containing appropriate assemblages of minerals. The results are commonly ambiguous, because of potential re-equilibration of touching minerals after diamond growth and possible ...
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A review and update of mantle thermobarometry for primitive arc magmas
American Mineralogist, 2017![][1] Erupted lavas and tephras remain among the best tools we have to ascertain the mantle processes that give rise to the compositional diversity and spatial distribution of near-primary magmas at volcanic arcs. A compilation of mantle-melt thermobarometry for natural, primitive arc magmas to date reveals published estimates vary between ~1000 ...
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Thermobarometry of ordinary chondrites
Doklady Earth Sciences, 2006N. G. Zinovieva +3 more
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Magma transport at Hawaii: Inferences based on igneous thermobarometry
Geology, 1997Pyroxene + liquid equilibrium in Hawaiian lavas occurs at a range of pressures for each volcano. Ranges are systematic and may be related to the stage of development of the magma conduit system. Kilauea, which is in its shield-building phase, yields relatively shallow storage estimates.
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Zircons: Age, Thermobarometry, and Source Inheritance
2021Dustin Trail +2 more
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