Weathering of quartz as an Archean climatic indicator
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Most researchers have doubted the isotopic inferences of persistently high Archean surface temperatures because the climate was sometimes cold enough for the glaciations, and chemical weathering of quartz from hot climates is lacking.
“Most researchers have doubted the isotopic inferences of persistently high Archean surface temperatures because the climate was sometimes cold enough for the aforementioned glaciations, and chemical weathering of quartz from hot climates is lacking (228).”
From The Archean atmosphere (2020) · cites this paper as [228]
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- Authors
- Sleep, N. H., & Hessler, A. M.
- Affiliations
- Stanford University (US)
- Grand Valley State University (US)
- Corresponding author
- Sleep, Norman H.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2006-01
- Volume
- 241
- Issue
- 3-4
- Pages
- 594-602
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2135234788
- Cited by
- 64
- References
- 45
- Citations by year
- 2026: 2 · 2025: 5 · 2024: 2 · 2023: 2 · 2021: 3 · 2020: 5 · 2019: 4 · 2018: 3 · 2017: 2 · 2016: 2 · 2014: 2 · 2013: 4 · 2012: 4
- FWCI
- 9.14
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- chert, paleothermometer, quartz dissolution, Moodies Group, granite weathering, clay formation, conglomerate provenance, early Earth climate, paleoclimate indicators
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