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Shock Metamorphism of Minerals

Elements (2012) 8 (1): 31-36.
This article has been cited by the following articles in journals that are participating in CrossRef Cited-by Linking.
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Microscopic evidence of stishovite generated in low-pressure shock experiments on porous sandstone: Constraints on its genesis
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Majoritic garnet grains within shock-induced melt veins in amphibolites from the Ries impact crater suggest ultrahigh crystallization pressures between 18 and 9 GPa
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Microstructural constraints on the mechanisms of the transformation to reidite in naturally shocked zircon
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Shocked monazite chronometry: integrating microstructural and in situ isotopic age data for determining precise impact ages
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CO2release due to impact devolatilization of carbonate: Results of shock experiments
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Revision and recalibration of existing shock classifications for quartzose rocks using low-shock pressure (2.5-20 GPa) recovery experiments and mesoscale numerical modeling
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Microspherules-Bearing White Sandstone: Implication of Cosmic Impact Event near Jurassic-Cretaceous Boundary in West Central Sinai, Egypt
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Impact origin of Archean cratons
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Halide based shock-wave treatment of fluid-rich natural phases
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Propagation of impact-induced shock waves in porous sandstone using mesoscale modeling
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The first MEMIN shock recovery experiments at low shock pressure (5-12.5 GPa) with dry, porous sandstone
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Diaplectic quartz glass and SiO2 melt experimentally generated at only 5 GPa shock pressure in porous sandstone: Laboratory observations and meso-scale numerical modeling
Earth and Planetary Science Letters (2013) 384: 17.
Shock Events in the Solar System: The Message from Minerals in Terrestrial Planets and Asteroids
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Petrology of impactites from El’gygytgyn crater: Breccias in ICDP-drill core 1C, glassy impact melt rocks and spherules
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Shock metamorphic features in quartz grains from the Saarijärvi and Söderfjärden impact structures, Finland
Meteoritics & Planetary Science (2013) 48 (6): 955.
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