9633498 Jacobsen Title: Abundances of W and Mo in MORBs: characterization of the depleted mantle reservoir. The composition of the Earth's mantle is the consequence of core formation, of mantle melting and liquid magma eruption, and of subduction and recycling of crust back into the mantle. The low abundance of some elements in the mantle is explained by their high solubility in the core. Some elements prefer silicate minerals and therefore are found in the mantle. Some elements do not prefer metal or minerals and are therefore concentrated in liquid magmas. The metals tungsten (W) and molybdenum (Mo) behave like metal- lovers and like liquid-lovers so their concentration in the lavas may tell much about the timing of the formation or the core. These metals are in such low abundance, however, that few quality analyses exist. This project will measure W and Mo in ocean floor basalt to understand the segregation of the Earth's core, mantle, and crust.

Agency
National Science Foundation (NSF)
Institute
Division of Ocean Sciences (OCE)
Type
Standard Grant (Standard)
Application #
9633498
Program Officer
David E. Epp
Project Start
Project End
Budget Start
1996-11-15
Budget End
1997-10-31
Support Year
Fiscal Year
1996
Total Cost
$50,000
Indirect Cost
Name
Harvard University
Department
Type
DUNS #
City
Cambridge
State
MA
Country
United States
Zip Code
02138