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Updated: Aug 8, 2025

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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High Mg# of the continental crust explained by calc-alkaline differentiation

Ming Tang1, Xuanyu Liu1, Kang Chen2

  • 1Key Laboratory of Orogenic Belt and Crustal Evolution, Ministry of Education; School of Earth and Space Sciences, Peking University, Beijing 100871, China.

National Science Review
|March 6, 2023
PubMed

Keywords:
Fe depletioncalc-alkaline differentiationcontinental crusthigh-Mg# andesiteslab melting

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