The Late Great Unconformity of the Central Canadian Shield
Abstract The Great Unconformity is a widely distributed surface separating Precambrian rocks from overlying Phanerozoic sedimentary sequences. The causes and implications of this feature, and whether it represents a singular global event, are much debated. Here, we present new apatite (U‐Th)/He (AHe...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Wiley
2021-06-01
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Series: | Geochemistry, Geophysics, Geosystems |
Subjects: | |
Online Access: | https://doi.org/10.1029/2020GC009567 |