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Aleutian Islands
Two‐Staged Rupture of the 19 October 2020 M w 7.6 Strike‐Slip Earthquake Illuminated the Boundary of Coupling Variation in the Shumagin Islands, Alaska
Double Seismic Zones along the Eastern Aleutian‐Alaska Subduction Zone Revealed by a High‐Precision Earthquake Relocation Catalog
Disentangling ecological and taphonomic signals in ancient food webs
The 1900 M w 7.6–8.0 Earthquake Offshore of Kodiak Island, Alaska
The eruptive history, magmatic evolution, and influence of glacial ice at long-lived Akutan volcano, eastern Aleutian Islands, Alaska, USA
Experimental constraints on the partial melting of sediment-metasomatized lithospheric mantle in subduction zones
Recent density decline in wild-collected subarctic crustose coralline algae reveals climate change signature
Evidence for frequent, large tsunamis spanning locked and creeping parts of the Aleutian megathrust
The robustness of Sr/Y and La/Yb as proxies for crust thickness in modern arcs
The Shumagin seismic gap structure and associated tsunami hazards, Alaska convergent margin
Coseismic Slip Model of the 2018 M w 7.9 Gulf of Alaska Earthquake and Its Seismic Hazard Implications
Archaean hydrothermal fluid modified zircons at Sunrise Dam and Kanowna Belle gold deposits, Western Australia: Implications for post-magmatic fluid activity and ore genesis
Gravity field, surface topography, and volcanic complexes of Kamchatka and its junction with the Aleutian arc
Abstract This paper synthesizes the framework and geological evolution of the Arctic Alaska–Chukotka microplate (AACM), from its origin as part of the continental platform fringing Baltica and Laurentia to its southward motion during the formation of the Amerasia Basin (Arctic Ocean) and its progressive modification as part of the dynamic northern palaeo-Pacific margin. A synthesis of the available data refines the crustal identity, limits and history of the AACM and, together with regional geological constraints, provides a tectonic framework to aid in its pre-Cretaceous restoration. Recently published seismic reflection data and interpretations, integrated with regional geological constraints, provide the basis for a new crustal transect (the Circum-Arctic Lithosphere Evolution (‘CALE’) Transect C) linking the Amerasia Basin and the Pacific margin along two paths that span 5100 km from the Lomonosov Ridge (near the North Pole), across the Amerasia Basin, Chukchi Sea and Bering Sea, and ending at the subducting Pacific plate margin in the Aleutian Islands. We propose a new plate tectonic model in which the AACM originated as part of a re-entrant in the palaeo-Pacific margin and moved to its present position during slab-related magmatism and the southward retreat of palaeo-Pacific subduction, largely coeval with the rifting and formation of the Amerasia Basin in its wake. Supplementary material: Supplementary material Plate 1 (herein referred to as Sup. Pl. 1) comprises Plate 1 and its included figures, which are an integral part of this paper. Plate 1 contains regional reflection-seismic-based cross sections and supporting material that collectively constitute CALE Transects C1 and C2 and form an important part of our contribution. Plate 1 is referred to in the text as Sup. Pl. 1, Transects C1 and C2 as Plate 1A and 1B, and plate figures as fig. P1.1, fig. P1.2, etc.). Supplementary material 2 contains previously unpublished geochronologic data on detrital zircon suites and igneous rocks. Supplementary material are available at https://doi.org/10.6084/m9.figshare.c.3826813