Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean
The amount of lead annually transferred from oceanic crust to metalliferous sediments was estimated in order to test the hypothesis that a non-magmatic flux of lead causes the Pb surplus in the continental crust. A Pb surplus has been inferred from global crust-mantle lead mass balances derived from...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1994
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.712126 https://doi.org/10.1594/PANGAEA.712126 |