Titlebook: Geomicrobiological Properties and Processes of Travertine; With a Focus on Japa Akihiro Kano,Tomoyo Okumura,Fumito Shiraishi Book 2019 Spri

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Introduction,one material. It was derived from . that means stone of Tivoli, an Italian town located 30?km east from Rome. Since Roman times, travertine has been used for popular stone material of buildings (e.g., .), sculpture, and tombs because the stone is relatively light, massive, and easy for cutting work.

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Basic Knowledge of Geochemical Processes, pressure (Ford and Pedley 1996; Gandin and Capezzuoli 2008, 2014; Capezzuoli et al. 2014). In this type of water, the active CO. degassing immediately after discharging on the ground increases pH and saturation state with respect to CaCO. of the water. Precipitation (and dissolution) of CaCO., whic

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主動(dòng)脈

Geomicrobiological Processes for Laminated Textures,ar. In lacustrine verves, regular seasonal changes in weather conditions accumulate a characteristic alternation of siliciclastic muddy particles and authigenic minerals. Based on patient search of the lamina counting and .C dating, time series of geochemical and paleontological proxies in the lacus

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Geochemical Model for Rapid Carbonate Precipitation of Travertines,, travertine can grow at a rate of tens of centimeters per year and tens of meters per a thousand years. Our founding strongly supports the previous statement that one of the most notable features of travertine is its rapid growth (or carbonate precipitation) rate (Kitano 1963; Folk et al. 1985; Pen

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Travertines in Japan, hot springs that developed calcareous deposits (Fig. 7.1, see also Figs. 7.13 and 7.15). Many of them are simple localities having only a single . facility, and an example is . hot spring on northern coast of the Honshu Island (Fig. 7.1), where you can see the beautiful sunset on the Japan Sea. . h

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https://doi.org/10.1007/978-1-4899-0545-1ot spring in Yamagata Prefecture is a relatively new geyser, and you have to drive 20?km on dirt road to reach there. Among the . listed on Fig. 7.1, only four locations, Masutomi, Shirahone, Arima, and Nagayu, have a large capacity and a wide facility for accepting many visitors. These . have also attracted many scientists for a study subject.