GSA Bulletin | GeoScienceWorld

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Volume 131,

Number 9-10,

September 2019

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

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Critical differences in sediment delivery and partitioning between marine and lacustrine basins: A comparison of marine and lacustrine aggradational to progradational clinothem pairs

Evidence for frequent, large tsunamis spanning locked and creeping parts of the Aleutian megathrust

The Ailao Shan−Red River shear zone revisited: Timing and tectonic implications

The lead-up to the Sturtian Snowball Earth: Neoproterozoic chemostratigraphy time-calibrated by the Tambien Group of Ethiopia

Organic carbon isotopes in terrestrial Permian-Triassic boundary sections of North China: Implications for global carbon cycle perturbations

Subduction initiation and back-arc opening north of Neo-Tethys: Evidence from the Late Cretaceous Torbat-e-Heydarieh ophiolite of NE Iran

LA-MC-ICP-MS U-Pb dating of low-U garnets reveals multiple episodes of skarn formation in the volcanic-hosted iron mineralization system, Awulale belt, Central Asia

Initiation and evolution of forearc basins in the Central Myanmar Depression

Extreme thermal metamorphism associated with Gondwana assembly: Evidence from sapphirine-bearing granulites of Rajapalayam, southern India

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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281 Sedimentation, earthquakes, and tsunamis in a shallow, muddy epeiric sea: Grinnell Formation (Belt Supergroup, ca. 1.45 Ga), western North America

206 The continental record and the generation of continental crust

166 Sedimentary evolution of the foreland basin in the NE Tibetan Plateau and the growth of the Qilian Shan since 7 Ma

162 Spatial and temporal trends in exhumation of the Eastern Himalaya and syntaxis as determined from a multitechnique detrital thermochronological study of the Bengal Fan

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

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