📣 Help Shape the Future of UKRI's Gateway to Research (GtR)

We're improving UKRI's Gateway to Research and are seeking your input! If you would be interested in being interviewed about the improvements we're making and to have your say about how we can make GtR more user-friendly, impactful, and effective for the Research and Innovation community, please email gateway@ukri.org.

Abiotic pyrite formation produces a large Fe isotope fractionation. (2011)

First Author: Guilbaud R
Attributed to:  Anoxic Transition Metal Isotope Geochemistry funded by NERC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1126/science.1202924

PubMed Identifier: 21700871

Publication URI: http://europepmc.org/abstract/MED/21700871

Type: Journal Article/Review

Volume: 332

Parent Publication: Science (New York, N.Y.)

Issue: 6037

ISSN: 0036-8075