Sulfide Aggregation in Ophiolitic Dunite Channels Explains Os‐Isotope Mismatch between Oceanic Crust and Mantle
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چکیده
منابع مشابه
Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust
The average chemical compositions of the continental crust and the oceanic crust (represented by MORB), normalized to primitive mantle values and plotted as functions of the apparent bulk partition coefficient of each element, form surprisingly simple, complementary concentration patterns. In the continental crust, the maximum concentrations are on the order of 50 to 100 times the primitive-man...
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ژورنال
عنوان ژورنال: Acta Geologica Sinica - English Edition
سال: 2020
ISSN: 1000-9515,1755-6724
DOI: 10.1111/1755-6724.14472