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Evolution of the Yangtze River network, southeastern Tibet: Insights from thermochronology and sedimentology
Loraine Gourbet; Rong Yang; Maria Giuditta Fellin; Jean-Louis Paquette; Sean D. Willett; JunFeng Gong; Colin Maden
Lithosphere December 12, 2019, Vol.12, 3-18. doi:https://doi.org/10.1130/L1104.1
Petrogenesis of Early Paleozoic high Sr/Y intrusive rocks from the North Qilian orogen: Implication for diachronous continental collision
Lithosphere December 19, 2019, Vol.12, 53-73. doi:https://doi.org/10.1130/L1129.1
Mesozoic denudation history of the lower Orange River and eastward migration of erosion across the southern African Plateau
Lithosphere January 30, 2020, Vol.12, 74-87. doi:https://doi.org/10.1130/L1121.1
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
Lithosphere January 30, 2020, Vol.12, 88-121. doi:https://doi.org/10.1130/L1115.1
Quantifying rates of “rifting while drifting” in the southern Gulf of California: The role of the southern Baja California microplate and its eastern boundary zone
Lithosphere February 12, 2020, Vol.12, 122-132. doi:https://doi.org/10.1130/L1132.1
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
Lithosphere January 30, 2020, Vol.12, 133-149. doi:https://doi.org/10.1130/L1142.1
Petrogenesis and tectonic setting of the Early Cretaceous granitoids in the eastern Tengchong terrane, SW China: Constraint on the evolution of Meso-Tethys
Lithosphere January 30, 2020, Vol.12, 150-165. doi:https://doi.org/10.1130/L1149.1
A non–plate tectonic model for the Eoarchean Isua supracrustal belt
Lithosphere January 30, 2020, Vol.12, 166-179. doi:https://doi.org/10.1130/L1130.1
Along-strike variations in sediment provenance within the Nanaimo basin reveal mechanisms of forearc basin sediment influx events
Daniel S. Coutts; William A. Matthews; Rebecca G. Englert; Morgan D. Brooks; Marie-Pier Boivin; Stephen M. Hubbard
Lithosphere February 12, 2020, Vol.12, 180-197. doi:https://doi.org/10.1130/L1138.1
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Cover Image
Cover Image
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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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