中文摘要：

Wenchuan 地震引起了作为碎片流动为未来动员提供丰富的 unconsolidated 材料的众多的山崩和倒塌。碎片流动将是很活跃的并且有一段时间在影响区域引起可观的损坏。因为与地震有关的环境变化，许多潜在地危险的碎片流动溪谷还得被识别。这份报纸作为学习区域从 Yinxiu 选择上面的 Min 河到 Wenchuan，解释 unconsolidated 存款，并且讨论他们到从差错的距离的关系。然后，使用那个信息和关于碎片流动出现的另外的因素的价值，潜在的碎片流动的地点被多因素分析全面鉴定和快速的鉴定。多因素全面鉴定采用模糊事元素扩展理论。在学习区域的 unconsolidated 材料的体积是大约 3.28 ?慦汵獴 吗？？

英文摘要：

The Wenchuan earthquake caused numerous landslides and collapses that provide abundant unconsolidated material for future mobilization as debris flows. Debris flows will be very active and cause considerable damage for some time in the affected area. Because of environmental changes related to the earthquake, many potentially dangerous debris flow gullies have yet to be identified. This paper selects the upper Min River from Yinxiu to Wenchuan as the study area, interprets the unconsolidated deposits, and discusses their relationship to distance from the fault. Then, applying that information and the values of other factors relating to debris flow occurrence, the locations of potential debris flows are analyzed by multi-factor comprehensive identification and rapid identification. The multi-factor comprehensive identification employs fuzzy matter-element extension theory. The volume of unconsolidated material in the study area is about 3.28 × 10^8 m3. According to the analysis by multi-factor comprehensive identification, 47 gullies have a high probability for potential debris flow, 8 gullies have a moderate probability, and 1 gully has a low probability.