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Titlebook: Elements and Mineral Resources; Joaquim Sanz,Oriol Tomasa,Nor Sidki-Rius Textbook 2022 The Editor(s) (if applicable) and The Author(s), un

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41#
發(fā)表于 2025-3-28 15:39:35 | 只看該作者
Carbon (C) [Z?=?6]A component of CO. gas, a pollutant causing global warming, acid rain, and climate change. Our civilization is constantly emitting large amounts of CO. from the combustion of fossil fuels (oil, coal, natural gas), in addition to natural emissions from volcanoes and animal and plant metabolism.
42#
發(fā)表于 2025-3-28 21:14:04 | 只看該作者
43#
發(fā)表于 2025-3-29 02:53:27 | 只看該作者
44#
發(fā)表于 2025-3-29 04:33:00 | 只看該作者
Cesium (Cs) [Z?=?55]The main source of cesium is pollucite, a primary lithium-cesium-rubidium mineral. It is also found in association with lithium-rich, lepidolite-bearing, and petalite-bearing zoned granite pegmatites.
45#
發(fā)表于 2025-3-29 09:25:33 | 只看該作者
Chromium (Cr) [Z?=?24]The primary mineral source of chromium (Cr) is chromite (Fe, Mg) Cr.O.. Chromite deposits can be classified into four deposit types: stratiform chromite; podiform chromite; placer chromite; and laterite.
46#
發(fā)表于 2025-3-29 11:59:04 | 只看該作者
https://doi.org/10.1007/978-3-662-62470-8te (NaCl), greater than 5%. The main halite deposits are saline flats characteristic of arid basins. They are shallow and dry apart from when storm flooding turns the saltpan and its surroundings into a temporary lake. Continental saline flats occupy the lowest areas of closed arid basins.
47#
發(fā)表于 2025-3-29 17:09:12 | 只看該作者
48#
發(fā)表于 2025-3-29 20:39:50 | 只看該作者
49#
發(fā)表于 2025-3-30 03:29:33 | 只看該作者
50#
發(fā)表于 2025-3-30 07:59:30 | 只看該作者
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