Kaigas
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- Insights Into Chemical Weathering of the Upper Continental Crust from the Geochemistry of Ancient Glacial Diamictites
- Global Neoproterozoic (Sturtian) Post
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- Compositional Evolution of the Upper Continental Crust Through Time, As Constrained by Ancient Glacial Diamictites
- A New Rock-Based Definition for the Cryogenian Period (Circa 720 – 635 Ma)
- Sheet-Crack Cements in Marinoan (635 Ma) Cap Dolostones As Regional Benchmarks of Vanishing Ice-Sheets
- Calibrating the Cryogenian Carbonate of the Basal Doushantuo Formation (635.2 T 0.2 Ma) (9); and Other Glacial Deposits Francis A
- Calibrating the Cryogenian Carbonate of the Basal Doushantuo Formation (635.2 T 0.2 Ma) (9); and Other Glacial Deposits Francis A
- Carbonates Bounding Glacial Deposits: Evidence For
- Two Long-Lasting Synchronous Neoproterozoic Glaciations
- Sedimentary Challenge to Snowball Earth
- Snowball Earth Ocean Chemistry Driven by Extensive Ridge Volcanism
- The Laurentian Neoproterozoic Glacial Interval
- Age Constraints on Precambrian Glaciations and the Subdivision of Neoproterozoic Time
- Hofmann-Namibia-Glaciations.Pdf
- Re-Os Geochronology and Coupled Os-Sr Isotope Constraints on the Sturtian Snowball Earth
- Re-Os Geochronology and Coupled Os-Sr Isotope Constraints on the Sturtian Snowball Earth
- Os Isotopic Systematics of the Upper Continental Crust Through Time: Evidence from Glacial Diamictites