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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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樓主: 快樂
11#
發(fā)表于 2025-3-23 11:08:48 | 只看該作者
12#
發(fā)表于 2025-3-23 16:25:33 | 只看該作者
https://doi.org/10.1007/978-981-13-1337-0Japanese Hot spring; Terrestrial carbonate; Hydrothermal stromatolite; Cyanobacteria; Sedimentary system
13#
發(fā)表于 2025-3-23 19:02:55 | 只看該作者
14#
發(fā)表于 2025-3-24 00:28:58 | 只看該作者
15#
發(fā)表于 2025-3-24 05:01:35 | 只看該作者
Rate Processes and Reaction Models,ed in Chap. ., the rapid sedimentation rate is closely associated with rapid CO. degassing from water, which elevates the level of supersaturation with respect for CaCO.. Intensity of the CO. degassing is generally related with hydrological conditions: more CO. degassing in turbulent conditions. The
16#
發(fā)表于 2025-3-24 09:45:39 | 只看該作者
https://doi.org/10.1007/978-3-319-57310-6 formational processes requires a wide range of analyses with macro-microscopic viewpoints. Microbiological influence to the textures of the carbonate precipitates is normally obscure in mesoscopic observation in field, but can be clearly examined by particular methods of microscopic observation. Si
17#
發(fā)表于 2025-3-24 13:09:44 | 只看該作者
Shia S. Kuan,George G. Guilbaultar. 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
18#
發(fā)表于 2025-3-24 16:15:54 | 只看該作者
19#
發(fā)表于 2025-3-24 20:39:07 | 只看該作者
https://doi.org/10.1007/978-1-4899-0545-1 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
20#
發(fā)表于 2025-3-25 01:09:31 | 只看該作者
Current flow: a non-equilibrium process, sedimentological features (Chap. .), and the analytical methods applied for travertine studies (Chap. .). After reviewing vital parts of the knowledge, we introduced a wide range of sedimentological, geochemical, and biological analyses performed mainly for the travertine in Japan. Our results brou
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