Tungsten isotope evidence from ∼3.8-Gyr metamorphosed sediments for early meteorite bombardment of the Earth View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2002-07

AUTHORS

Ronny Schoenberg, Balz S. Kamber, Kenneth D. Collerson, Stephen Moorbath

ABSTRACT

The 'Late Heavy Bombardment' was a phase in the impact history of the Moon that occurred 3.8 4.0 Gyr ago, when the lunar basins with known dates were formed. But no record of this event has yet been reported from the few surviving rocks of this age on the Earth. Here we report tungsten isotope anomalies, based on the (182)Hf (182)W system (half-life of 9 Myr), in metamorphosed sedimentary rocks from the 3.7 3.8-Gyr-old Isua greenstone belt of West Greenland and closely related rocks from northern Labrador, Canada. As it is difficult to conceive of a mechanism by which tungsten isotope heterogeneities could have been preserved in the Earth's dynamic crust mantle environment from a time when short-lived (182)Hf was still present, we conclude that the metamorphosed sediments contain a component derived from meteorites. More... »

PAGES

403

Journal

TITLE

Nature

ISSUE

6896

VOLUME

418

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/nature00923

DOI

http://dx.doi.org/10.1038/nature00923

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1005213180

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/12140554


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148 schema:name †Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK
149 rdf:type schema:Organization
 




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