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Discovery of a major negative 13C spike in the Carnian (Late Triassic) linked to the eruption of Wrangellia flood basalts (2011)

First Author: Dal Corso J

Attributed to: National Environmental Isotope Facility (NEIF) funded by NERC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1130/g32473.1

Publication URI: http://dx.doi.org/10.1130/g32473.1

Type: Journal Article/Review

Parent Publication: Geology

Issue: 1