Mass Fractions of S, Cu, Se, Mo, Ag, Cd, In, Te, Ba, Sm, W, Tl and Bi in Geological Reference Materials and Selected Carbonaceous Chondrites Determined by Isotope Dilution <scp>ICP</scp>‐<scp>MS</scp>
Zaicong Wang(China University of Geosciences), Frank Wombacher(University of Bonn), Harry Becker(Ruhr University Bochum)
Cited by 64
Related Papers
Highly siderophile element composition of the Earth’s primitive upper mantle: Constraints from new data on peridotite massifs and xenoliths
|Geochimica et Cosmochimica Acta|2006|599
Comparative 187Re-187Os systematics of chondrites
|Geochimica et Cosmochimica Acta|2002|285
Trace element fractionation during dehydration of eclogites from high-pressure terranes and the implications for element fluxes in subduction zones
|Chemical Geology|2000|275
Rhodium, gold and other highly siderophile element abundances in chondritic meteorites
|Geochimica et Cosmochimica Acta|2009|232