Resolving the age of the Haughton impact structure using coupled 40Ar/39Ar and U-Pb geochronology

The Haughton Dome located on Devon Island, in the Canadian Archipelago represents a well-preserved, moderate-sized, complex impact crater. Previous age constraints for the 24 km-diameter impact structure have ranged from ca. 21 Ma to ca. 39 Ma. Herein, we present a coordinated microstructural and in...

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Bibliographic Details
Published in:Geochimica et Cosmochimica Acta
Main Authors: Erickson, Timmons, Kirkland, Chris, Jourdan, Fred, Schmieder, M., Hartnady, Michael, Cox, Morgan A., Timms, Nick
Format: Article in Journal/Newspaper
Language:English
Published: PERGAMON-ELSEVIER SCIENCE LTD 2021
Subjects:
Science & Technology
Physical Sciences
Geochemistry & Geophysics
Shock metamorphism
Zircon
Monazite
U-Pb
40Ar/39Ar
INDUCED HYDROTHERMAL ACTIVITY
CANYON SANIDINE STANDARD
SHOCK-WAVE METAMORPHISM
K-40 DECAY CONSTANTS
DEVON-ISLAND
ISOTOPIC COMPOSITION
JOINT DETERMINATION
IMPROVED ACCURACY
ARGON DIFFUSION
K-AR
Devon Island
Haughton Dome
Canadian Archipelago
Online Access:https://hdl.handle.net/20.500.11937/90162
https://doi.org/10.1016/j.gca.2021.04.008
Description
Summary:The Haughton Dome located on Devon Island, in the Canadian Archipelago represents a well-preserved, moderate-sized, complex impact crater. Previous age constraints for the 24 km-diameter impact structure have ranged from ca. 21 Ma to ca. 39 Ma. Herein, we present a coordinated microstructural and in situ U-Pb study of zircon and monazite coupled with 40Ar/39Ar laser step heating of shock-melted K-feldspar clasts from shock metamorphosed gneissic fragments collected from the allochthonous impact breccia at Haughton. Moderately shocked zircon and monazite grains yield an age distribution consistent with an Archean protolith metamorphosed at ca. 1.9 Ga, whereas shock recrystallized zircon and monazite yield a lower intercept age of 31.8 ± 1.7 Ma (n = 48, MSWD = 0.58, P = 0.99). Four inverse isochron 40Ar/39Ar ages of shocked feldspar clasts yield a weighted mean age of 31.04 ± 0.37 Ma (MSWD = 0.98, P = 0.40), within uncertainty of the U-Pb lower concordia intercept. Ar diffusion modelling supports the interpretation of the impact age and helps resolve impact-driven age resetting. These results highlight the power of coupling multiple geochronologic techniques for determining impact ages, especially from targets with complex geologic histories. Furthermore, they resolve previous discrepancies in the age of the Haughton Dome and the interpretation of the post impact stratigraphy of the crater fill.

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