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中文摘要：
<正>地幔源区岩性是控制地幔部分熔融过程中微量元素行为的重要因素。近十年来,第一周期过渡族元素(FRTEs,First Row Transition Elements)被广泛应用于地幔源区岩性识别。超基性、基性岩石部分熔融过程中,FRTEs表现为相容到中等不相容,是追踪地幔源区岩性的有力工具(Le Roux et al.,2011)。Humayun et al.(2004)精确测定了夏威夷玄武质熔岩、冰岛苦橄岩以及大洋中脊玄武质玻璃
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