带来
发表于 2025-3-25 03:57:02
Using QTM to support map generalization,Walter Benjamin verstand sich als Kritiker, freilich als einen, der mit seiner Kritik zugleich philosophiert und in anspruchsvollem Sinne literarisch tätig ist.
GEST
发表于 2025-3-25 10:29:14
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ANT
发表于 2025-3-25 13:14:36
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一再遛
发表于 2025-3-25 18:20:08
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按等级
发表于 2025-3-26 00:03:13
Front Matters material existed as a completely amorphous colloidal complex. However, many mineralogists thought that clays could be a mixture, containing varying proportions of crystalline material (Mackenzie, 1963). The mixed-oxide hypothesis of van Bemmelen (1910), associating the colloidal state with non-cry
无意
发表于 2025-3-26 00:34:27
,Walter Benjamin — Versuch einer Würdigung, therapeutic properties and medicinal applications.Thought-pThis book provides a comprehensive description of the application of clay minerals as disinfectants and the ingredients of medicines. While the presently available literature highlights one or two aspects of medicinal clays, a comprehensive
文件夹
发表于 2025-3-26 07:56:11
,“Nur mein Herze brach”,n are rarely totally absent from these environmeents (e.g., Griffin 1963, Stone and Siegel 1969). Except on muddy tidal flats and in some coastal depressions, clay particles are usually swept away, which was enhanced in late Quaternary periods by hydrodynamic variations linked to sea-level changes.
BLINK
发表于 2025-3-26 11:39:04
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词汇
发表于 2025-3-26 14:16:00
,“Verschränkung von Natur und Geschichte” Zur ldee der ‘Naturgeschichte” bei Benjamin und Adorno,physical or chemical exchanges between the clay- bearing material and the human body, respectively. Physical therapies involve energy exchanges that can be induced during a massage by employing mechanical pressure on the previously heated (maximum at 45–50°C) clay pack, and from the pressure and hea
rods366
发表于 2025-3-26 20:07:59
,Von der allegorischen Lektüre zur ldee der “integralen Prosa”, also represent the most fascinating component of this complex “chemical world”, because they carry records of many discrete evolutionary events in the constantly changing history of the upper crust. Isotopic data gathered from analyses of clay minerals can, therefore, serve as very useful tracers f