Crossmark

Geology and lithogeochemistry of hydrothermal mudstones from the upper block near the Duck Pond volcanogenic massive sulfide (VMS) deposit, Newfoundland, Canada: evidence for low-temperature venting into oxygenated mid-Cambrian seawater

Crossref DOI link: https://doi.org/10.1007/s00126-018-0795-3

Published Online: 2018-02-26

Published Print: 2018-12

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Piercey, Stephen J.

Squires, Gerry

Brace, Terry
Funding

Funding for this research was provided by:

NSERC Discovery Grant

Aur Resources/ Teck Resources Ltd.

NSERC Collaborative Research and Development Grant

Canadian Mining Industry Research Organization

NSERC Industrial Research Chair

Altius Resources Inc.
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Article History

Received: 1 March 2017

Accepted: 31 January 2018

First Online: 26 February 2018

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