Abstract:The second decade of the 21st century (2010-2020) is a decade of vigorous developments in mineralogy, petrology and geochemistry in China of various fields from the craton destruction to orogenic belt evolution and from the continental to oceanic lithospheres, is a decade of comprehensive march from the depth to breadth, and is also a decade of the development from catching up to surpassing in mineralogical, petrological and geochemical researches. In the past decade, the mineralogists, petrologists and geochemists in China have made many breakthroughs in mineralogy, petrology and geochemistry of the mantle. These advances are mainly focused on two aspects including those of researches on direct samples of the mantle, such as mantle mineralogy, continental and oceanic lithospheres, peridotite of orogenic belt, and water in mantle; and those of researches on samples of magmatic rocks derived from the mantle, such as continental and oceanic basalts, basic and ultrabasic complexes, and igneous carbonatite. In particular, the development and wide application of new methods for analyzing non-traditional stable isotopes or metal stable isotopes (such as Li, Mg, Fe and Ca isotopes, etc.) have greatly promoted the research progress of mantle petrology and geochemistry in China, and achieved a historic leap from catching up to surpassing in researches on petrology and geochemistry of the manle.
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