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Provenance of Pennsylvanian–Permian sedimentary rocks associated with the Ancestral Rocky Mountains orogeny in southwestern Laurentia: Implications for continental-scale Laurentian sedime...
Ryan J. Leary; Paul Umhoefer; M. Elliot Smith; Tyson M. Smith; Joel E. Saylor; Nancy Riggs; Greg Burr; Emma Lodes; Daniel Foley; Alexis Licht; Megan A. Mueller; Chris Baird
Cretaceous and late Cenozoic uplift of a Variscan Massif: The case of the French Massif Central studied through low-temperature thermochronometry
Valerio Olivetti; Maria Laura Balestrieri; Vincent Godard; Olivier Bellier; Cécile Gautheron; Pierre G. Valla; Massimiliano Zattin; Claudio Faccenna; Rosella Pinna-Jamme; Kevin Manchuel
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Cover Image
Cover Image
COVER: View to the southwest of the Isua supracrustal belt from the northeastern extremity of the belt. The edge of the Greenland ice sheet is shown on the left. In the foreground, chert and banded iron formation display pencil cleavage that is a significant element of the paper. In the distant center, the high hills behind the lakes comprise a ~3.7 Ga tonalite body. See “A non–plate tectonic model for the Eoarchean Isua supracrustal belt” by A. Alexander G. Webb, Thomas Müller, Jiawei Zuo, Peter J. Haproff, and Anthony Ramí rez-Salazar, https://doi.org/10.1130/L1130.1.
PHOTO BY: Peter J. Haproff
COVER DESIGN BY: Heather L. Sutphin
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