Issues
ARTICLES
High-resolution record of multiple organic carbon-isotope excursions in lacustrine deposits of Upper Sinemurian through Pliensbachian (Early Jurassic) from the Sichuan Basin, China
Contrasting mechanisms and timescales of subduction and exhumation as recorded by Paleoproterozoic and late Paleozoic high-pressure granulites in the North China Craton
Two-stage exhumation of deeply subducted continental crust: Insight from zircon, titanite, and apatite petrochronology, Sulu belt of eastern China
Locating Lhasa terrane in the Rodinia and Gondwana supercontinents: A key piece of the reconstruction puzzle
Kinematic evolution of the central Andean retroarc thrust belt in northwestern Argentina and implications for coupling between shortening and crustal thickening
(U-Th)/He chronology: Part 1. Data, uncertainty, and reporting
(U-Th)/He chronology: Part 2. Considerations for evaluating, integrating, and interpreting conventional individual aliquot data
Geological history and supercontinent cycles of the Arctic
Compositional and metamorphic controls on tectonic erosion along a continental subduction-collision zone: Implications from mafic granulites in the northern Sulu orogen
Recognition of late Paleoproterozoic gold mineralization in the North China craton: Evidence from multi-mineral U-Pb geochronology and stable isotopes of the Shanggong deposit
Modification of the lithospheric mantle induced by recycled crustal components: Insights from Early Cretaceous appinites from the Liaodong Peninsula, NE China
Spatially averaged stratigraphic data to inform watershed sediment routing: An example from the Mid-Atlantic United States
Strontium isotope stratigraphy and LA-ICP-MS U-Pb carbonate age constraints on the Cenozoic tectonic evolution of the southern South China Sea
Fingerprinting the metal source and cycling of the world’s largest antimony deposit in Xikuangshan, China
Featured Neoarchean granitoid association in the central North China Craton: An indicator of warm plate subduction
Cenozoic deformation in the eastern domain of the North Qaidam thrust belt, northern Tibetan Plateau
Correlation between South China and India and development of double rift systems in the South China–India Duo during late Neoproterozoic time
Ediacaran magmatism and rifting along the northern margin of the Tarim craton: Implications for the late Neoproterozoic Rodinia configuration and breakup
Diatom evidence for a groundwater divide that limited the extent of Lake Estancia, New Mexico, USA, highstands during the Last Glacial Maximum
Environmental conditions and mechanisms restricting microbial methanogenesis in the Miquan region of the southern Junggar Basin, NW China
Detrital zircon provenance and transport pathways of Pleistocene-Holocene eolian sediment in the Pampean Plains, Argentina
Sedimentology of the latest Permian to Early Triassic in the terrestrial settings of the North China Basin: Low-latitude climate change during a warming-driven crisis
A one-million-year isotope record from siderites formed in modern ferruginous sediments
Unusual δ26Mg values in oceanic crust basalts from the South China Sea
Disequilibrium river networks dissecting the western slope of the Sierra Nevada, California, USA, record significant late Cenozoic tilting and associated surface uplift: Comment
Disequilibrium river networks dissecting the western slope of the Sierra Nevada, California, USA, record significant late Cenozoic tilting and associated surface uplift: Reply
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Cover Image
Cover Image
Cover: Michigan's tallest waterfall, Houghton-Douglass Falls, cascades 110 feet (34 m) over Mesoproterozoic basaltic lavas of North America's Midcontinent Rift System. Older Portage Lake Volcanics at the falls have been thrust over softer younger Jacobsville Sandstone along the Keweenaw fault, which extends along the entire Keweenaw Peninsula where such waterfalls are common. Flows and interflow sedimentary layers in the hanging wall host native copper deposits, once the main source of copper for the United States. Attractive building stone from durable parts of sandstone in the footwall was used in construction throughout the Eastern United States, including the famed original Waldorf-Astoria Hotel in New York City. See “Detached structural model of the Keweenaw fault system, Lake Superior region, North America: Implications for its origin and relationship to the Midcontinent Rift System” by DeGraff and Carter, p. 449–466.
Photo by: Alexis Dahl.
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