Based on value chain analysis method,we surveyed and interviewed interest groups of batik industry in Danzhai County.From raw material production,product processing,marketing,organization and management,we discussed t...Based on value chain analysis method,we surveyed and interviewed interest groups of batik industry in Danzhai County.From raw material production,product processing,marketing,organization and management,we discussed the supply chain of batik products in ethnic minority areas,and analyzed favorable factors of batik industry development and obstacles to interest groups developing batik industry.Finally,we put forward corresponding policy suggestions,including strengthening farmers' ability in batik production section,enhancing capability construction of batik cooperatives and associations,increasing cultural value added of batik products,bolster policy and financial support of government departments,and promoting establishment of cooperative mechanism for handicrafts.展开更多
In 2016,the Geological Brigade No.103 of Guizhou Geology and Mineral Exploration and Development Bureau discovered two super-large manganese deposits at Pujue and Taoziping,in Songtao County,Guizhou Province（Fig.1）....In 2016,the Geological Brigade No.103 of Guizhou Geology and Mineral Exploration and Development Bureau discovered two super-large manganese deposits at Pujue and Taoziping,in Songtao County,Guizhou Province（Fig.1）.The Pujue manganese deposit has191.59 million tons of proven（332＋333）class ore reserves,including 35.54 million tons of 332 class and展开更多
Based on GIS,RS and the landscape analysis software,landscape changes in the middle and lower reaches of Houzhai River in Puding County of Guizhou Province from 1973 to 2004 were analyzed.The results indicated that pa...Based on GIS,RS and the landscape analysis software,landscape changes in the middle and lower reaches of Houzhai River in Puding County of Guizhou Province from 1973 to 2004 were analyzed.The results indicated that paddy fields and dry fields held a dominant status.In the change of landscape types,forest land reduced continually,dry fields changed complicatedly,and the mutual transformation among grass land,shrub land and forest land was obvious.The area of bare rock increased remarkably in the slope range between 10° and 35°.Artificially 'returning cultivation land into forests and pastures','reclamation by damaging forests and pastures',and natural ecosystem converse succession existed at the same time.Therefore,the whole landscape was in an unstable state.展开更多
Karst rocky desertification is one of the major ecological and environmental problems that threaten the sustainable development of southwestern China. It is caused by irrational and intensive land-use patterns in kars...Karst rocky desertification is one of the major ecological and environmental problems that threaten the sustainable development of southwestern China. It is caused by irrational and intensive land-use patterns in karst geo-ecological environment. Therefore, it is vital to identify how human forces work on this degraded environment. Based on the soil erosion information in 2000 and remote sensing images of Guanling County collected in 2000 and 2007, four grades of karst rocky desertification data in 14 villages of Guanling County were extracted. Impacts of population, affluence, and other human forces on karst rocky desertification were analyzed using STIRPAT model. The results show that:1) Factors of population and affluence had strong influence on karst rocky desertification. In the STIRPAT model analysis, the population and affluence coefficients were positive, indicating that the increase in population and affluence would lead to more serious desertification. 2) Factors of farmer correlated with karst rocky desertification negatively, especially the way of viewing the relationship between people and nature, and the level of knowledge about rocky desertification. Government behavior was not a significant factor in this analysis. 3) The findings provide evidence that STIRPAT model can be used to analyze the relationship between human driving forces and rocky desertification.展开更多
At present,targeted poverty alleviation is a major development strategy in China.Based on the investigation of Danzhai County in Guizhou Province,this paper argues that industry development is the fundamental measure ...At present,targeted poverty alleviation is a major development strategy in China.Based on the investigation of Danzhai County in Guizhou Province,this paper argues that industry development is the fundamental measure through which to implement the poverty alleviation program.Industry development includes both the development of local industries in povertystricken areas and the development of industries in other regions of China.Local development is mainly achieved when the invisible superior resources become visible and the notable superior resources are capitalized in povertystricken areas,in which,the capitalization of factors and resources relies on fundamental governmental investments which will create a profit space for the poverty-stricken areas through the down-to-countryside cadres' precise guidance for the use of poverty alleviation funds to help identify a breakthrough for industry development,and particularly the attempts to focus on the development of high-end industries under the lower-end production mode to form a community with common interests aiding poverty alleviation.Development in other regions can be mainly achieved through various modes such as "tax-finance-poverty alleviation," "industry-employment-poverty alleviation" and "industry-enterprise direct investment-poverty alleviation" to offer indirect or direct support for poverty alleviation in poverty-stricken areas.An appropriate handling is required to deal with many problems related to the local industry development in targeted poverty alleviation and the targeted poverty alleviation in industry development.展开更多
Emplacement ages, geochemical characteristics and analysis of continental dynamics on gabbroic intrusions in Luodian County, Guizhou Province, have been discussed based on studies of isotopic chronology （the whole-ro...Emplacement ages, geochemical characteristics and analysis of continental dynamics on gabbroic intrusions in Luodian County, Guizhou Province, have been discussed based on studies of isotopic chronology （the whole-rock Sm-Nd and Rb-Sr isochron methods）, major elements, trace elements and PGE. Intrusive activities of the gabbroic intrusions in the study area took place during the Late Yanshanian Orogenic Movement （the Cretaceous Period）, as indicated by the Sm-Nd isochron ages （t）=（99.6±4.5） （2σ） Ma and by the Rb-Sr isochron ages t=（97±1.6） （2σ） Ma. The gabbroic intrusions are attached to mafic rocks in cal-alkaline basaltic series. They occurred as dikes and might be formed under an extensional background of the continent. Differentiation of their magmatic crystallization resulted in obvious zonation of petrography. In the gabbroic intrusions of this study, large ion lithophile elements and LREE are enriched, and the chondrite-normalized REE distribution pattern is leftward inclined without anomalies of JCe or JEu, and there are high concentrations of PGE and ratios of Pd/Ir （averaging 4.21）. All of these imply that their source areas may be basaltic magma in the upper mantle with high-level partial melting, derived from EMl-type enriched mantle. It is different from Emeishan basalt, which may be related to the upper mantle at low-grade partial melting. Emplacement mechanism of the gabbroic intrusions in this study may suppose to be asthenosphere upheaving as an isolated hot wave in the presence of mantle fluid, resulting in basaltic magma intruded into the continental crust as a diapiric intrusion. Therefore, uplifting of faulting-block and extensional deformation could take place in the shallow part of the continental crust while vertical amassing and accretion of magmatic materials in the deep part of the continental crust. These special processes could supposed to be a special background of continental dynamics for this large-scale epithermal metallogenic domain, such as Au, As, Sb and Hg deposits, and vertical uplifting of the Yunnan-Guizhou Plateau in the Cretaceous Period.展开更多
基金Supported by Doctor Scientific Research Project of Guizhou Normal University(Strategy for Relationship between Establishing Resourcebased Enterprises and Harmonious Development of Local Communities-A Case Study of Sino Guizhou Jinfeng Mining Co.,Ltd.)
文摘Based on value chain analysis method,we surveyed and interviewed interest groups of batik industry in Danzhai County.From raw material production,product processing,marketing,organization and management,we discussed the supply chain of batik products in ethnic minority areas,and analyzed favorable factors of batik industry development and obstacles to interest groups developing batik industry.Finally,we put forward corresponding policy suggestions,including strengthening farmers' ability in batik production section,enhancing capability construction of batik cooperatives and associations,increasing cultural value added of batik products,bolster policy and financial support of government departments,and promoting establishment of cooperative mechanism for handicrafts.
文摘In 2016,the Geological Brigade No.103 of Guizhou Geology and Mineral Exploration and Development Bureau discovered two super-large manganese deposits at Pujue and Taoziping,in Songtao County,Guizhou Province（Fig.1）.The Pujue manganese deposit has191.59 million tons of proven（332＋333）class ore reserves,including 35.54 million tons of 332 class and
文摘Based on GIS,RS and the landscape analysis software,landscape changes in the middle and lower reaches of Houzhai River in Puding County of Guizhou Province from 1973 to 2004 were analyzed.The results indicated that paddy fields and dry fields held a dominant status.In the change of landscape types,forest land reduced continually,dry fields changed complicatedly,and the mutual transformation among grass land,shrub land and forest land was obvious.The area of bare rock increased remarkably in the slope range between 10° and 35°.Artificially 'returning cultivation land into forests and pastures','reclamation by damaging forests and pastures',and natural ecosystem converse succession existed at the same time.Therefore,the whole landscape was in an unstable state.
基金Under the auspices of National Natural Science Foundation of China(No.40801039,40801066,41001183)
文摘Karst rocky desertification is one of the major ecological and environmental problems that threaten the sustainable development of southwestern China. It is caused by irrational and intensive land-use patterns in karst geo-ecological environment. Therefore, it is vital to identify how human forces work on this degraded environment. Based on the soil erosion information in 2000 and remote sensing images of Guanling County collected in 2000 and 2007, four grades of karst rocky desertification data in 14 villages of Guanling County were extracted. Impacts of population, affluence, and other human forces on karst rocky desertification were analyzed using STIRPAT model. The results show that:1) Factors of population and affluence had strong influence on karst rocky desertification. In the STIRPAT model analysis, the population and affluence coefficients were positive, indicating that the increase in population and affluence would lead to more serious desertification. 2) Factors of farmer correlated with karst rocky desertification negatively, especially the way of viewing the relationship between people and nature, and the level of knowledge about rocky desertification. Government behavior was not a significant factor in this analysis. 3) The findings provide evidence that STIRPAT model can be used to analyze the relationship between human driving forces and rocky desertification.
基金sponsored by the Cooperative Innovation Center of Chinese Characterized Socialist Economic Construction
文摘At present,targeted poverty alleviation is a major development strategy in China.Based on the investigation of Danzhai County in Guizhou Province,this paper argues that industry development is the fundamental measure through which to implement the poverty alleviation program.Industry development includes both the development of local industries in povertystricken areas and the development of industries in other regions of China.Local development is mainly achieved when the invisible superior resources become visible and the notable superior resources are capitalized in povertystricken areas,in which,the capitalization of factors and resources relies on fundamental governmental investments which will create a profit space for the poverty-stricken areas through the down-to-countryside cadres' precise guidance for the use of poverty alleviation funds to help identify a breakthrough for industry development,and particularly the attempts to focus on the development of high-end industries under the lower-end production mode to form a community with common interests aiding poverty alleviation.Development in other regions can be mainly achieved through various modes such as "tax-finance-poverty alleviation," "industry-employment-poverty alleviation" and "industry-enterprise direct investment-poverty alleviation" to offer indirect or direct support for poverty alleviation in poverty-stricken areas.An appropriate handling is required to deal with many problems related to the local industry development in targeted poverty alleviation and the targeted poverty alleviation in industry development.
文摘Emplacement ages, geochemical characteristics and analysis of continental dynamics on gabbroic intrusions in Luodian County, Guizhou Province, have been discussed based on studies of isotopic chronology （the whole-rock Sm-Nd and Rb-Sr isochron methods）, major elements, trace elements and PGE. Intrusive activities of the gabbroic intrusions in the study area took place during the Late Yanshanian Orogenic Movement （the Cretaceous Period）, as indicated by the Sm-Nd isochron ages （t）=（99.6±4.5） （2σ） Ma and by the Rb-Sr isochron ages t=（97±1.6） （2σ） Ma. The gabbroic intrusions are attached to mafic rocks in cal-alkaline basaltic series. They occurred as dikes and might be formed under an extensional background of the continent. Differentiation of their magmatic crystallization resulted in obvious zonation of petrography. In the gabbroic intrusions of this study, large ion lithophile elements and LREE are enriched, and the chondrite-normalized REE distribution pattern is leftward inclined without anomalies of JCe or JEu, and there are high concentrations of PGE and ratios of Pd/Ir （averaging 4.21）. All of these imply that their source areas may be basaltic magma in the upper mantle with high-level partial melting, derived from EMl-type enriched mantle. It is different from Emeishan basalt, which may be related to the upper mantle at low-grade partial melting. Emplacement mechanism of the gabbroic intrusions in this study may suppose to be asthenosphere upheaving as an isolated hot wave in the presence of mantle fluid, resulting in basaltic magma intruded into the continental crust as a diapiric intrusion. Therefore, uplifting of faulting-block and extensional deformation could take place in the shallow part of the continental crust while vertical amassing and accretion of magmatic materials in the deep part of the continental crust. These special processes could supposed to be a special background of continental dynamics for this large-scale epithermal metallogenic domain, such as Au, As, Sb and Hg deposits, and vertical uplifting of the Yunnan-Guizhou Plateau in the Cretaceous Period.
