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David Green has been adept at selecting significant petrological observations or hypotheses and devising experimental strategies to investigate them. He has studied a wide range of topics, including mineral assemblages of peridotites and basalts at high pressures, the experimental calibration of mineral geothermometers and geobarometers, the reasons for compositional variability of basaltic magmas including the roles of carbon and hydrogen, the genesis of carbonatite magmas, the identification of carbonatite metasomatism in the Earth’s lithosphere, the origins of and relationships among lunar basalts, and the nature of the lunar interior.
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JOURNAL OF THE AMERICAN ACADEMY OF ORTHOPAEDIC SURGEONSno. 13 (2022): 581-585
Applied Phycologyno. 1 (2021): 41-59
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