Metamorphism of eucrite meteorites studied quantitatively using induced thermoluminescence

Statistics – Applications

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Basalt, Metamorphism (Geology), Meteoritic Composition, Thermoluminescence, Chondrites, Feldspars, Igneous Rocks, Lunar Rocks, Metamorphic Rocks, Meteorites, Eucrites, Metamorphism, Thermoluminescence, Achondrites, Samples, Meteorite, Laboratory Studies, Stony Meteorites, Basalt, Techniques, Classification, Catalog, Igneous Rocks, Thermal History, Antarctic Meteorites, Parent Bodies, Yamato Meteorites, Lew Meteorites, Pca Meteorites, Eet Meteorites, Alh Meteorites, Petrology

Scientific paper

Induced thermoluminescence studies provide a new and quantitative means of determining relative metamorphic intensities for eucrite meteorites, the simplest and most ancient products of basaltic volcanism. Using this technique, it is shown that the eucrites constitute a continuous metamorphic series and not, as commonly assumed, two groups of metamorphosed and nonmetamorphosed meteorites. It is suggested that the method may have applications to other basalts.

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