Issues
Articles
A link between rift-related volcanism and end-Ediacaran extinction? Integrated chemostratigraphy, biostratigraphy, and U-Pb geochronology from Sonora, Mexico
Heterogeneous mantle-derived helium isotopes in the Canary Islands and other ocean islands
Time scales of syneruptive volatile loss in silicic magmas quantified by Li isotopes
Passive-margin magmatism caused by enhanced slab-pull forces in central Tibet
High transient stress in the lower crust: Evidence from dry pseudotachylytes in granulites, Lofoten Archipelago, northern Norway
Similar Holocene glaciation histories in tropical South America and Africa
Ancient Adélie penguin colony revealed by snowmelt at Cape Irizar, Ross Sea, Antarctica
Redefining East African Rift System kinematics
Implications of giant ooids for the carbonate chemistry of Early Triassic seawater
Temporary late Holocene barrier-chain deterioration due to insufficient sediment availability, Wadden Sea, Denmark
The deep magmatic cumulate roots of the Acadian orogen, eastern North America
Paleomagnetic constraints on the duration of the Australia-Laurentia connection in the core of the Nuna supercontinent
A bigger splat: The catastrophic geology of a 1.2-b.y.-old terrestrial megaclast, northwest Scotland
Rapid emplacement of massive Duluth Complex intrusions within the North American Midcontinent Rift
The formation of continental roots
Dendritic reidite from the Chesapeake Bay impact horizon, Ocean Drilling Program Site 1073 (offshore northeastern USA): A fingerprint of distal ejecta?
Longest continuously erupting large igneous province driven by plume-ridge interaction
Soft sediment deformation in dry pyroclastic deposits at Ubehebe Crater, Death Valley, California
Thin crème brûlée rheological structure for the Eastern California Shear Zone
Microbial sulfate reduction plays an important role at the initial stage of subseafloor sulfide mineralization
Fragmentation of South China from greater India during the Rodinia-Gondwana transition
Detrital zircon populations of the eastern Laurentian margin in the Appalachians
Erratum
ERRATUM: Minimal net incision of the northern Sierra Nevada (California, USA) since the Eocene–early Oligocene
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Cover Image
Cover Image
COVER: Oblique view of crudely folded sandstone injectite breccia overlying the Clachtoll fault (northwest Scotland) located just above the yellow meter ruler. The breccia formed as an ~250 kt megaclast of Archaean Lewisian basement gneisses fell onto, and overpressured, wet sediments of the Mesoproterozoic Stoer Group, possibly following an earthquake at ca. 1.2 Ga. The local shortening represented by the Clachtoll fault and overlying fold likely occurred immediately following impact, as the megacalst slid sideways to the left prior to its passive burial below younger sandstones of the basal Stoer Group, which are visible in the background. See “A bigger splat: The catastrophic geology of a 1.2-b.y.-old terrestrial megaclast, northwest Scotland” by Killingback et al., p. 180–184.
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