Sequestration of atmospheric CO2 in a weathering-derived, serpentinite-hosted magnesite deposit: 14C tracing of carbon sources and age constraints for a refined genetic model

Author:

Oskierski H.C.,Dlugogorski B.Z.,Jacobsen G.

Funder

AINSE

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference92 articles.

1. Origin of ultramafic-hosted vein magnesite deposits;Abu-Jaber;Ore Geol. Rev.,1992

2. Paleozoic ophiolitic assemblages within the southern New England Orogen of eastern Australia: implications for growth of the Gondwana margin;Aitchison;Tectonics,1994

3. Age profile of ophiolitic rocks across the late Paleozoic New England Orogen, New South Wales: implications for tectonic models;Aitchison;Aust. J. Earth Sci.,1995

4. New and revised lithostratigraphic units from the southwestern New England Fold Belt;Aitchison;Geol. Surv. NSW Quart. Notes,1988

5. Factors and processes governing the 14C content of carbonate in desert soils;Amundson;Earth Planet. Sci. Lett.,1994

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