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Geology May 01, 2022, Vol.50, 531. doi:https://doi.org/10.1130/GEOL50THMAY.1
Non-steady-state slip rates emerge along evolving restraining bends under constant loading
Geology February 03, 2022, Vol.50, 532-536. doi:https://doi.org/10.1130/G49745.1
Boron proxies record paleosalinity variation in the North American Midcontinent Sea in response to Carboniferous glacio-eustasy
Wei Wei; Wenchao Yu; Thomas J. Algeo; Achim D. Herrmann; Lian Zhou; Jinhua Liu; Qian Wang; Yuansheng Du
Geology February 11, 2022, Vol.50, 537-541. doi:https://doi.org/10.1130/G49521.1
Ultrahigh-temperature granites and a curious thermal eye in the post-collisional South Bohemian batholith of the Variscan orogenic belt (Europe)
Geology February 11, 2022, Vol.50, 542-546. doi:https://doi.org/10.1130/G49645.1
Final inversion of the Midcontinent Rift during the Rigolet Phase of the Grenvillian Orogeny
Eben B. Hodgin; Nicholas L. Swanson-Hysell; James M. DeGraff; Andrew R.C. Kylander-Clark; Mark D. Schmitz; Andrew C. Turner; Yiming Zhang; Daniel A. Stolper
Geology February 11, 2022, Vol.50, 547-551. doi:https://doi.org/10.1130/G49439.1
What drives Fe depletion in calc-alkaline magma differentiation: Insights from Fe isotopes
Geology February 11, 2022, Vol.50, 552-556. doi:https://doi.org/10.1130/G49705.1
Reconciling persistent sub-zero temperatures in the McMurdo Dry Valleys, Antarctica, with Neogene dynamic marine ice-sheet fluctuations
Geology February 11, 2022, Vol.50, 557-561. doi:https://doi.org/10.1130/G49664.1
Implications for Ediacaran biological evolution from the ca. 602 Ma Lantian biota in China
Geology February 11, 2022, Vol.50, 562-566. doi:https://doi.org/10.1130/G49734.1
Coriolis effect recorded in Late Pleistocene Marine Isotope Stage 5e Bahamian aeolianites
Geology February 11, 2022, Vol.50, 567-571. doi:https://doi.org/10.1130/G49454.1
Reassessment of ocean paleotemperatures during the Late Ordovician
Geology February 11, 2022, Vol.50, 572-576. doi:https://doi.org/10.1130/G49422.1
Giant sheath-folded nappe stack demonstrates extreme subhorizontal shear strain in an Archean orogen
Geology February 25, 2022, Vol.50, 577-582. doi:https://doi.org/10.1130/G49599.1
Long-lasting viscous drainage of eclogites from the cratonic lithospheric mantle after Archean subduction stacking
Geology February 25, 2022, Vol.50, 583-587. doi:https://doi.org/10.1130/G49793.1
Decrypting the polymetamorphic record of the Himalaya
Geology February 25, 2022, Vol.50, 588-592. doi:https://doi.org/10.1130/G49467.1
Zn-, Mg- and O-isotope evidence for the origin of mantle eclogites from Roberts Victor kimberlite (Kaapvaal Craton, South Africa)
Geology February 25, 2022, Vol.50, 593-597. doi:https://doi.org/10.1130/G49780.1
No effect of thermal maturity on the Mo, U, Cd, and Zn isotope compositions of Lower Jurassic organic-rich sediments
Alexander J. Dickson; Erdem Idiz; Don Porcelli; Melissa J. Murphy; Ricardo Celestino; Hugh C. Jenkyns; Simon W. Poulton; Stephen P. Hesselbo; John N. Hooker; Micha Ruhl; Sander H.J.M. van den Boorn
Geology February 25, 2022, Vol.50, 598-602. doi:https://doi.org/10.1130/G49724.1
Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA
Geology February 25, 2022, Vol.50, 603-609. doi:https://doi.org/10.1130/G49925.1
Tibetan Plateau growth linked to crustal thermal transitions since the Miocene
Geology February 25, 2022, Vol.50, 610-614. doi:https://doi.org/10.1130/G49534.1
The continent-to-ocean transition in the Iberia Abyssal Plain
Ingo Grevemeyer; Cesar R. Ranero; Cord Papenberg; Valenti Sallares; Rafael Bartolomé; Manel Prada; Luis Batista; Marta Neres
Geology February 25, 2022, Vol.50, 615-619. doi:https://doi.org/10.1130/G49753.1
Quantifying large-scale continental shelf margin growth and dynamics across middle-Cretaceous Arctic Alaska with detrital zircon U-Pb dating
Geology March 08, 2022, Vol.50, 620-625. doi:https://doi.org/10.1130/G49118.1
Shallow distributed faulting in the Imperial Valley, California, USA
Geology March 08, 2022, Vol.50, 626-630. doi:https://doi.org/10.1130/G49572.1
Linking metamorphism and plate boundaries over the past 2 billion years
Geology March 08, 2022, Vol.50, 631-635. doi:https://doi.org/10.1130/G49637.1
Hot atmospheric formation of carbonate accretionary lapilli at the Cretaceous-Paleogene boundary, Brazos River, Texas, from clumped isotope thermometry
Geology March 08, 2022, Vol.50, 636-640. doi:https://doi.org/10.1130/G49674.1
Forum
Could the Réunion plume have thinned the Indian craton? — COMMENT
Geology May 01, 2022, Vol.50, e548. doi:https://doi.org/10.1130/G49940C.1
Widespread glasses generated by cometary fireballs during the late Pleistocene in the Atacama Desert, Chile: COMMENT
Pierrick Roperch; Jérôme Gattacceca; Millarca Valenzuela; Bertrand Devouard; Jean-Pierre Lorand; Pierre Rochette; Claudio Latorre; Pierre Beck
Geology May 01, 2022, Vol.50, e550. doi:https://doi.org/10.1130/G49958C.1
Could the Réunion plume have thinned the Indian craton? — REPLY
Geology May 01, 2022, Vol.50, e549. doi:https://doi.org/10.1130/G50124Y.1
Widespread glasses generated by cometary fireballs during the late Pleistocene in the Atacama Desert, Chile: REPLY
Geology May 01, 2022, Vol.50, e551. doi:https://doi.org/10.1130/G50144Y.1
Early Earth zircons formed in residual granitic melts produced by tonalite differentiation: REPLY
Geology May 01, 2022, Vol.50, e553. doi:https://doi.org/10.1130/G50170Y.1
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Cover Image
Cover Image
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COVER: Aerial view looking northeast at Sunset Bay State Park (foreground) and Coos Bay (background) along the southwestern Oregon coast (USA). East-dipping sandstones and mudstones of the middle Eocene Coaledo Formation provide exceptional exposures of a prograding storm- and wave-dominated deltaic sequence adjacent to the inboard Coos Bay Coal Field, where lignitic coals accumulated under tropical conditions during the Eocene ‘Hothouse’ climate. These rocks and the underlying fluvio-deltaic Tyee Formation were deposited just prior to the onset of Ancestral Cascades arc magmatism; their widespread exposure across the southern Oregon Coast Range today is due to crustal thickening and exhumation since Oligocene time. See ‘Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA’ by Darin et al., p. 603–609.
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