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Volume 95, Number 3
June 2025
Journal of Sedimentary Research Cover Image for Volume 95, Issue 3
ISSN: 1527-1404
EISSN: 1938-3681
In this Issue
Grain size matters: late Quaternary dynamics of a sediment-routing system in Canterbury Basin, South Island, New Zealand
Tania Villaseñor; John M. Jaeger; Kathleen M. Marsaglia; Jasmyn Nolasco; Carrie Bender-Whitaker; Claire Bailey
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Experimental development of chlorite: insights from a kaolinite precursor
Abdulwahab Muhammad Bello; Anas Muhammad Salisu; Abduljamiu Olalekan Amao; Mustapha Umar; Khalid Al-Ramadan
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A petrologically constrained timeframe for early dolomitization in the mixed carbonate–siliciclastic Miocene Dam Formation, Qatar
Mohammed Al-Musawi; John M. Rivers; Stephen E. Kaczmarek
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Research Article

Constant size and mobility of grains in the Oligo-Miocene megafan deposits in the Swiss Molasse Basin despite long-term changes in tectonic processes, climatic conditions, and sediment fl...
Philippos Garefalakis; Fritz Schlunegger; Ariel Henrique Do Prado; David Mair; Alexander C. Whittaker
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Volcanism and climate recorded in giant grains from dust of the late Paleozoic Panthalassic Ocean
Patrick R. Kelly; Hiroyoshi Sano; Katsumi Ueno; Vladimir I. Davydov; Nicholas G. Heavens; Lindsey E. Hunt; James D. Gleason; Gerilyn S. Soreghan
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Temperatures of albitization of plagioclase in sandstones from the Norwegian continental shelf
Olav Walderhaug; Kristin W. Porten
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THE EDITORS’ PAGE

The Editors’ Page
Steve Kaczmarek; Dustin Sweet; Melissa Lester
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  • Cover Image

    Cover Image

    issue cover

    Cover Photo: Well-rounded quartz grains (left; ~ 200 µm diameter) and vesicular rhyolitic glass (~ 100 µm diameter) extracted from carbonates of the Akiyoshi terrane, Japan. The Akiyoshi carbonates formed in the equatorial Panthalassic ocean, thousands of kilometers from the continental and felsic-volcanic sources that supplied these wind-transported giant grains.

All Issues
  • Online ISSN 1938-3681
  • ISSN 1527-1404
  • Copyright © 2025 SEPM Society for Sedimentary Geology
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