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https://hdl.handle.net/11499/46695
Title: | Non-marine carbonate: Wherefore art thou? | Authors: | Capezzuoli, Enrico Della Porta, Giovanna Rogerson, Mike Tagliasacchi, Ezher |
Publisher: | Wiley | Abstract: | Introduction of the special issue on non-marine carbonates. (A) Sub-lacustrine spring pinnacles from alkaline Mono Lake (California, USA); scale is 2 m. (B) Cascade tufa from Sarikavak (TK); scale is 175 cm. (C) Travertine deposits from Pamukkale (TK); scale is 170 cm. (D) Speleothems and flowstones from Kaklik Cave (TK); hammer for scale. (E) Temporarily exposed microbial bioherms at Bridger Bay shoreline, Antelope Island, Great Salt Lake (Utah, USA); sedimentologists for scale. (F) Upper Jurassic rhizolite laminar calcrete (base at hammer edge) from Rochaforte (Portugal; courtesy of V.P. Wright; Wright & Azeredo, 2006). (G) The Brook Bottom leachate deposit (Harpur Hill, Derbyshire, UK). Anthropocene carbonate deposit forming downstream of a legacy deposit of impure lime, left by historical industrial activity at the site (courtesy of Laura Bastianini); scale is about 10 m. | URI: | https://doi.org/10.1002/dep2.170 https://hdl.handle.net/11499/46695 |
ISSN: | 2055-4877 |
Appears in Collections: | Mühendislik Fakültesi Koleksiyonu Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection |
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The Depositional Record - 2021 - Capezzuoli.pdf | 721.58 kB | Adobe PDF | View/Open |
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