熄灭
发表于 2025-3-28 16:22:53
NATO Science Series B:http://image.papertrans.cn/l/image/588851.jpg
Physiatrist
发表于 2025-3-28 19:23:10
978-1-4757-1401-2Springer Science+Business Media New York 1975
allergen
发表于 2025-3-29 00:08:19
Low-Dimensional Cooperative Phenomena978-1-4757-1399-2Series ISSN 0258-1221
遭受
发表于 2025-3-29 05:52:51
ted landslides or in slow-moving landslides of such clay. This is due to loss of the physical and/or chemical bonds provided by the salt, demonstrating the physic-chemical effect of pore water on the shear strength of the clay. However, is there a similar effect when such clay is subjected to undrai
意外
发表于 2025-3-29 10:47:27
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PAGAN
发表于 2025-3-29 15:28:18
M. J. Ricemmunity. Identification of landslide-prone zones is mandatory for developing land use plans in regions affected by landslides. Landslide susceptibility maps are crucial for mapping landslide hazards and evaluating the risk resulting from landslides. Zones susceptible to the geologic phenomenon of la
Pelvic-Floor
发表于 2025-3-29 17:44:13
W. A. Littlenomic losses. In areas with steep topography, the temporal and spatial clustering of long-duration, moderate-to-short-duration high-intensity rainfall contributes to landslides. Shifting precipitation patterns due to climate change, alterations to sub-surface conditions, such as pore-water pressures
考得
发表于 2025-3-29 20:14:39
Zoltán G. Soosf the granite, caused by cooling and tectonic phases, originated 4 main joint sets, regularly spaced (few decimeters to meters). Several slope instability phenomena have been identified and classified according to mechanism, material involved and state of activity. They are mainly related to rock fa
积习已深
发表于 2025-3-30 03:01:53
Jan Kommandeurf the granite, caused by cooling and tectonic phases, originated 4 main joint sets, regularly spaced (few decimeters to meters). Several slope instability phenomena have been identified and classified according to mechanism, material involved and state of activity. They are mainly related to rock fa
强化
发表于 2025-3-30 07:03:08
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