trigger
发表于 2025-3-25 06:49:52
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cajole
发表于 2025-3-25 09:14:39
https://doi.org/10.1007/978-3-662-12648-6Clays; Erden; Erosion; Sediment; Sedimentation; Ton; Umwelt; diagenesis; environment; mineralogy; soil
flex336
发表于 2025-3-25 13:18:42
978-3-642-08195-8Springer-Verlag Berlin Heidelberg 1995
在前面
发表于 2025-3-25 15:53:38
Geology of Clays,creation of clays, the transformation of clays and the destruction of clays in different geological environments. Clays, as is the case for most objects on the Earth, are ephemeral. They have a life span which is governed by their geologic history. Clays occur under a limited range of conditions in
支架
发表于 2025-3-25 21:32:18
Composition and Mineralogy of Clay Minerals,2 μm. This limit was imposed by the use of the petrographic microscope where the smallest particle which could be distinguished optically was of this size. Clays were essentially those minerals which could not be dealt with in a conventional nineteenth century manner. Chemical analyses were neverthe
整顿
发表于 2025-3-26 01:22:51
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SOBER
发表于 2025-3-26 05:15:00
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残酷的地方
发表于 2025-3-26 12:07:41
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古代
发表于 2025-3-26 14:01:30
Hydrothermal Alteration by Veins,etamor-phic, magmatic) have percolated. Chemical interactions with rocks along these pathways produce secondary minerals among which phyllosilicates are usually the dominant species. The mineral deposit sealing the fracture and the altered wall rocks are described as hydrothermal veins. These veins
Fulminate
发表于 2025-3-26 18:58:35
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