Hadean Zircon Petrochronology
Abstract
Research Article| August 01, 2017 Hadean Zircon Petrochronology T. Mark Harrison; T. Mark Harrison Department of Earth, Planetary and Space Sciences, University of California, Los Angeles, Los Angeles, CA 90095, USA Search for other works by this author on: GSW Google Scholar Elizabeth A. Bell; Elizabeth A. Bell Department of Earth, Planetary and Space Sciences, University of California, Los Angeles, Los Angeles, CA 90095, USA Search for other works by this author on: GSW Google Scholar Patrick Boehnke Patrick Boehnke Department of Earth, Planetary and Space Sciences, University of California, Los Angeles, Los Angeles, CA 90095, USA Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2017) 83 (1): 329–363. https://doi.org/10.2138/rmg.2017.83.11 Article history first online: 10 Nov 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation T. Mark Harrison, Elizabeth A. Bell, Patrick Boehnke; Hadean Zircon Petrochronology. Reviews in Mineralogy and Geochemistry 2017;; 83 (1): 329–363. doi: https://doi.org/10.2138/rmg.2017.83.11 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search The inspiration for this volume arose in part from a shift in perception among U–Pb geochronologists that began to develop in the late 1980s. Prior to then, analytical geochronology emphasized progressively lower blank analysis of separated accessory mineral aggregates (e.g., Krogh 1982; Parrish 1987), with results generally interpreted to reflect a singular moment in time. For example, a widespread measure of confidence in intra-analytical reliability was conformity to an MSWD (a form of χ2 test; Wendt and Carl 1991) of unity. This approach implicitly assumed that geological processes act on timescales that are short with respect... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Analysis of zircons suggests that continents, oceans, and perhaps life all originated in the Hadean.
“analysis of zircons—crystals of zirconium silicate (ZrSiO4)—suggests that continents, oceans, and perhaps life all originated in the Hadean (16).”
From The Archean atmosphere (2020) · cites this paper as [16]
At the end of the Hadean, Earth had oceans, continents, an anoxic atmosphere likely rich in CO2 and N2, and probably life.
“In summary, at the end of the Hadean, Earth had oceans, continents (16), an anoxic atmosphere likely rich in CO2 and N2, and probably life (Fig. 1).”
From The Archean atmosphere (2020) · cites this paper as [16]
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Zircon: The Metamorphic Mineral
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Experimentally determined Si isotope fractionation between zircon and quartz
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The Oldest Terrestrial Mineral Record
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Progress in the principle and application of zircon trace element
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Self-citationMaking continental crust on water-bearing terrestrial planets
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Evidence of Eoarchean crust beneath the Yakutian kimberlite province in the Siberian craton
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Evidence for oceans pre-4300 Ma confirmed by preserved igneous compositions in Hadean zircon
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Archean Cratons: Time Capsules of the Early Earth
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Hadean Jack Hills Zircon Geochemistry
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Self-citationThe evolution of Earth’s early continental crust
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Biogeodynamics: Coupled evolution of the biosphere, atmosphere, and lithosphere
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Contemporaneous mobile- and stagnant-lid tectonics on the Hadean Earth
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An accessory mineral and experimental perspective on the evolution of the early crust
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Of zircons and zircons: The tumultuous story of Zr-Hf and REE during cooling of peralkaline granites
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Exploiting Friedel pairs to interpret scanning 3DXRD data from complex geological materials
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Oxidized Hadean magmas and Archean mobile-lid tectonics revealed by Jack Hills zircon
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Is Deep Time Geology Scientific?
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Plate Boundary Interactions Through Geologic History
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Self-citationPlanetary Impacts: Friend or Foe?
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- Authors
- Harrison, T. M., Bell, E. A., & Boehnke, P.
- Affiliations
- University of California, Los Angeles (US)
- Venue
- Reviews in Mineralogy and Geochemistry
- Publisher
- Mineralogical Society of America
- Published
- 2017-02-01
- Volume
- 83
- Issue
- 1
- Pages
- 329-363
- ISSN
- 1529-6466 (ISSN-L)
- OpenAlex
- W2617338718
- Cited by
- 97
- References
- 212
- Citations by year
- 2026: 13 · 2025: 7 · 2024: 15 · 2023: 8 · 2022: 6 · 2021: 10 · 2020: 15 · 2019: 10 · 2018: 7 · 2017: 6
- FWCI
- 7.41
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Reviews in Mineralogy and Geochemistry (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Mineralogy and Gemology Studies
- Keywords
- Hadean zircon, U-Pb geochronology, early Earth, zircon inclusions, zircon oxygen isotopes
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