Deformational history and thermochronology of Wrangel Island, East Siberian Shelf and coastal Chukotka, Arctic Russia
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Elizabeth L. Miller, V. V. Akinin, T. A. Dumitru, E. S. Gottlieb, M. Grove, K. Meisling, G. Seward, 2018. "Deformational history and thermochronology of Wrangel Island, East Siberian Shelf and coastal Chukotka, Arctic Russia", Circum-Arctic Lithosphere Evolution, V. Pease, B. Coakley
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Abstract
In Arctic Russia, south of Wrangel Island, Jura–Cretaceous fold belt structures are cut by c. 108–100 Ma plutonic rocks and a c. 103 Ma migmatitic complex (U–Pb, zircon) that cooled by c. 96 Ma (40Ar/39Ar biotite); the structures are unconformably overlain by c. 88 Ma and younger (U–Pb, zircon) volcanic rocks. Wrangel Island, with a similar stratigraphy and added exposure of Neoproterozoic basement rocks, was thought to represent the westwards continuation of the Jura–Cretaceous Brookian thrust belt of Alaska. A penetrative, high-strain, S-dipping foliation formed during north–south stretching in Triassic and older rocks, with stretched pebble aspect ratios of c. 2:1:0.5 to 10:1:0.1. Deformation was at greenschist facies (chlorite+white mica; biotite at depth; temperature c. 300–450°C). Microstructures suggest deformation mostly by pure shear and north–south stretching; the quartz textures and lattice preferred orientations suggest temperatures of c. 300–450°C. 40Ar/39Ar K-feldspar spectra (n = 1) and muscovite (n = 3) (total gas ages c. 611–514 Ma) in Neoproterozoic basement rocks are consistent with a short thermal pulse during deformation at 105–100 Ma. Apatite fission track ages (n = 7) indicate cooling to near-surface conditions at c. 95 Ma. The shared thermal histories of Wrangel Island and Chukotka suggest that Wrangel deformation is related to post-shortening, north–south extension, not to fold–thrust belt deformation. Seismic data (line AR-5) indicate a sharp Moho and strong sub-horizontal reflectivity in the lower and middle crust beneath the region. Wrangel Island probably represents a crustal-scale extensional boudin between the North Chukchi and Longa basins.
Supplementary material: Sample localities, details of the analytical methods, data tables and the full discussion of the results of electron back-scatter diffraction studies of quartz lattice preferred orientations are available at https://doi.org/10.6084/m9.figshare.c.3741272
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Contents
Circum-Arctic Lithosphere Evolution
CONTAINS OPEN ACCESS
GeoRef
- absolute age
- Ar/Ar
- Arctic Ocean
- Arctic region
- Asia
- Chukotka Russian Federation
- coastal environment
- Commonwealth of Independent States
- Cretaceous
- crust
- deformation
- East Siberian Sea
- electron diffraction data
- fission-track dating
- fold and thrust belts
- geochronology
- geophysical profiles
- magmatism
- marine environment
- melting
- Mesozoic
- methods
- microstructure
- models
- outcrops
- petrography
- Russian Arctic
- Russian Federation
- seismic profiles
- shelf environment
- structural analysis
- thermal history
- thermochronology
- U/Pb
- velocity structure
- Wrangel Island
- Crystalnaya River