The newly-discovered Xiyi lead-zinc deposit is a large deposit located in the north central Baoshan block of the southern Sanjiang metallogenic belt section, Southwest China.The surface of the deposit is mainly covere...The newly-discovered Xiyi lead-zinc deposit is a large deposit located in the north central Baoshan block of the southern Sanjiang metallogenic belt section, Southwest China.The surface of the deposit is mainly covered by eluvial-deluvial lateritic layer, without any mineralized outcrops. The main concealed orebody V3 is buffed in the depth of 300-500m. The orebodies are controlled by certain stratigraphic horizons, and most are cut by strata with a high angle, while a few occur along the strata. The direct wall rocks are calcisiltite, calclithite, bioclastic calcarenite,展开更多
Using Google Earth software as a platform,this study has established an integrated database of both old and new landslides in Baoshan City,Yunnan Province,China,and analyzed their development characteristics together ...Using Google Earth software as a platform,this study has established an integrated database of both old and new landslides in Baoshan City,Yunnan Province,China,and analyzed their development characteristics together with distribution rules,respectively.Based on the results,a total of 2427 landslides occurred in the study area,including 2144 new landslides and 283 old landslides,with a total area of about104.8 km^2.The new landslides are mostly in small-scales with an area less than 10000 m^2,while the area of individual old landslide is mostly larger than 10000 m^2.By analyzing the relationship between the two types of landslides and eight impact factors(i.e.,elevation,slope angle,slope aspect,slope position,lithology,fault,regional Peak Ground Acceleration(PGA),and average annual rainfall),the different individual influencing factors,distribution regularities and mechanisms of the two types of landslides are revealed.In detail,the main influencing factors of new landslides are elevation,slope angle,slope aspect,slope position,lithology,regional PGA and average annual rainfall,while the influencing factors of old landslides are mainly elevation,slope angle,and lithology.This study provides basic data and support for landslide assessment and further disaster reduction in Baoshan City.Besides,it also provides new constraints in deeply understanding the effect of different topographic and geological conditions,historical earthquakes,rainfall and other factors on the occurrence mechanisms of both new landslides and old landslides.展开更多
文摘The newly-discovered Xiyi lead-zinc deposit is a large deposit located in the north central Baoshan block of the southern Sanjiang metallogenic belt section, Southwest China.The surface of the deposit is mainly covered by eluvial-deluvial lateritic layer, without any mineralized outcrops. The main concealed orebody V3 is buffed in the depth of 300-500m. The orebodies are controlled by certain stratigraphic horizons, and most are cut by strata with a high angle, while a few occur along the strata. The direct wall rocks are calcisiltite, calclithite, bioclastic calcarenite,
基金sponsored by the ScientificResearch Fund of Institute of Engineering Mechanics,China Earthquake Administration(2017QJGJ05-03)the National Natural Science Foundation of China(41941016)。
文摘Using Google Earth software as a platform,this study has established an integrated database of both old and new landslides in Baoshan City,Yunnan Province,China,and analyzed their development characteristics together with distribution rules,respectively.Based on the results,a total of 2427 landslides occurred in the study area,including 2144 new landslides and 283 old landslides,with a total area of about104.8 km^2.The new landslides are mostly in small-scales with an area less than 10000 m^2,while the area of individual old landslide is mostly larger than 10000 m^2.By analyzing the relationship between the two types of landslides and eight impact factors(i.e.,elevation,slope angle,slope aspect,slope position,lithology,fault,regional Peak Ground Acceleration(PGA),and average annual rainfall),the different individual influencing factors,distribution regularities and mechanisms of the two types of landslides are revealed.In detail,the main influencing factors of new landslides are elevation,slope angle,slope aspect,slope position,lithology,regional PGA and average annual rainfall,while the influencing factors of old landslides are mainly elevation,slope angle,and lithology.This study provides basic data and support for landslide assessment and further disaster reduction in Baoshan City.Besides,it also provides new constraints in deeply understanding the effect of different topographic and geological conditions,historical earthquakes,rainfall and other factors on the occurrence mechanisms of both new landslides and old landslides.