Titlebook: Low-Dimensional Cooperative Phenomena; The Possibility of H H. J. Keller Book 1975 Springer Science+Business Media New York 1975

熄滅

NATO Science Series B:http://image.papertrans.cn/l/image/588851.jpg

Physiatrist

978-1-4757-1401-2Springer Science+Business Media New York 1975

allergen

Low-Dimensional Cooperative Phenomena978-1-4757-1399-2Series ISSN 0258-1221

遭受

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

PAGAN

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

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

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

積習(xí)已深

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

強(qiáng)化