GSA Bulletin | GeoScienceWorld

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Volume 132,

Number 7-8,

1 July 2020

IF: 3.970, 5-year IF: 4.708 Scopus: 2.24 SJR, 134 H Index

New Online

Spatiotemporal patterns of distributed slip in southern Owens Valley indicated by deformation of late Pleistocene shorelines, eastern California

Generation of Late Cretaceous Ji’an basalts through asthenosphere-slab interaction in South China

Thermotectonic evolution of the Paleozoic granites along the Shangdan suture zone (central China): Crustal growth and differentiation by magma underplating in an orogenic belt

Interpreting and reporting ⁴⁰Ar/³⁹Ar geochronologic data

Geochemistry of contrasting stream types, Taylor Valley, Antarctica

Provenance of early Paleozoic sedimentary rocks in the Altyn Tagh orogen: Insights into the paleoposition of the Tarim craton in northern Gondwana associated with final closure of the Proto−Tethys Ocean

U-Pb detrital zircon ages of Cambrian−Ordovician sandstones from the Taebaeksan Basin, Korea: Provenance variability in platform shelf sequences and paleogeographic implications

Biomarker evidence of algal-microbial community changes linked to redox and salinity variation, Upper Devonian Chattanooga Shale (Tennessee, USA)

Triassic−Jurassic evolution of the eastern North China Craton: Insights from the Lushun-Dalian area, South Liaodong Peninsula, NE China

About the Journal

Geological Society of America Bulletin is a leading international journal for major scholarly research in all branches of the earth sciences. Published continuously since 1890. Full-text available for all issues.

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393 Interpreting and reporting ⁴⁰Ar/³⁹Ar geochronologic data

295 The Capitanian (Guadalupian, Middle Permian) mass extinction in NW Pangea (Borup Fiord, Arctic Canada): A global crisis driven by volcanism and anoxia

254 Controls on the formation of microbially induced sedimentary structures and biotic recovery in the Lower Triassic of Arctic Canada

219 Granite: From genesis to emplacement

141 Large igneous provinces and silicic large igneous provinces: Progress in our understanding over the last 25 years

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