Variation in the strontium isotopic composition of seawater (8 Ma to present) : Implications for chemical weathering rates and dissolved fluxes to the oceans-Reference-Cited by-同舟云学术

Variation in the strontium isotopic composition of seawater (8 Ma to present) : Implications for chemical weathering rates and dissolved fluxes to the oceans

Published:1990-10 Issue:4 Volume:80 Page:291-307
ISSN:0168-9622
Container-title:Chemical Geology: Isotope Geoscience section
language:en
Short-container-title:Chemical Geology: Isotope Geoscience section

Author:

Hodell David A.,Mead Gregory A.,Mueller Paul A.

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference53 articles.

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2. Paleomagnetism of sediments collected during Leg 90, southwest Pacific;Barton;Init. Rep. Sea Drill. Proj.,1986

3. Erosion of the Laurentide region of North America by glacial and glaciofluvial processes;Bell;Quat. Res.,1985

4. The Neogene Part 2. Neogene geochronology and chronostratigraphy;Berggren,1985

5. The Global Water Cycle;Berner,1987

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