The Ganzi geothermal field is located in the Songpan-Ganzi orogenic belt in Sichuan Province.Many hot springs are exposed along the Yalahe valley in Ganzi geothermal field,which is a favorable area for hightemperature...The Ganzi geothermal field is located in the Songpan-Ganzi orogenic belt in Sichuan Province.Many hot springs are exposed along the Yalahe valley in Ganzi geothermal field,which is a favorable area for hightemperature geothermal resource exploration.However,the geological model of heat exchange,the regional structure controlling hydrothermal convection and the development model of geothermal reservoirs are still unclear.Therefore,further studies are necessary to meet the geothermal exploration requirements in the middle and deep strata of this geothermal field.In this study,a geological model of the geothermal system of Ganzi geothermal field is proposed.We are convinced that there exists a hydrothermal convection system in the Ganzi geothermal field,the heat transfer of which is accomplished through deep-rooted major faults.Therefore,the identification of deep-rooted major faults and the description of geothermal reservoirs are the research objects of the integrated geophysical methods.The main factors controlling the geothermal reservoirs in the deep-rooted Xianshuihe major fault and Yalahe fault zones are analyzed by using gravity,aeromagnetic,and electromagnetic methods and techniques.The analysis results of regional gravity and aeromagnetic anomalies show that the Xianshuihe major fault has produced obvious gravity and aeromagnetic anomalies on the surface,and thus the position and strike of this fault can be accurately predicted by inversion of the aeromagnetic anomalies.Geothermal reservoirs show low-resistivity anomalies in the electromagnetic profile.The inversion results of the controlled source audio-frequency magnetotelluric(CSAMT)data show that geothermal reservoirs are mainly developed along the Yalahe valley,and the west side of the valley is more favorable for geothermal exploration.This study is of guiding significance to the efficient exploitation and utilization of the Ganzi geothermal field.展开更多
Major, trace and rare earth element （REE） concentrations of Late Triassic sediments （fine- grained sandstones and mudstones） from Hongcan Well 1 in the NE part of the Songpan-Ganzi Basin, western China, are used t...Major, trace and rare earth element （REE） concentrations of Late Triassic sediments （fine- grained sandstones and mudstones） from Hongcan Well 1 in the NE part of the Songpan-Ganzi Basin, western China, are used to reveal weathering, provenance and tectonic setting of inferred source areas. The Chemical Index of Alteration （CIA） reflects a low to moderate degree of chemical weathering in a cool and somewhat dry climate, and an A-CN-K plot suggests an older upper continental crust prove- nance dominated by felsic to intermediate igneous rocks of average tonalite composition. Based on the various geochemical tectonic setting discrimination diagrams, the Late Triassic sediments are inferred to have been deposited in a back-arc basin situated between an active continental margin （the Kunlun- Qinling Fold Belt） and a continental island arc （the Yidun Island Arc）. The Triassic sediments in the study area underwent a rapid erosion and burial in a proximal slope-basin environment by the petrographic data,while the published flow directions of Triassic turbidites in the Aba-Zoige region was not supported Yidun volcanic arc source. Therefore, we suggest that the Kunlun-Qinling terrane is most likely to have supplied source materials to the northeast part of the Songpan-Ganzi Basin during the Late Triassic.展开更多
Based on the statistical data of daily precipitation in 14 meteorological stations of Ganzi Prefecture from 1960 to 2011, the temporal variation characteristics of precipitation in Ganzi Prefecture in nearly 50 years ...Based on the statistical data of daily precipitation in 14 meteorological stations of Ganzi Prefecture from 1960 to 2011, the temporal variation characteristics of precipitation in Ganzi Prefecture in nearly 50 years were studied. The results showed that in Ganzi Prefecture, annual precipitation showed an increasing trend, and averaged 659 mm in nearly 50 years, mainly varying from 550 to 750 mm. In a year, precipitation was mainly distributed in summer and autumn, and the precipitation in summer and autumn accounted for 83% of annual precipitation. Seen from the interdecadal variation of annual precipitation, annual precipitation in Ganzi Prefecture showed an increasing trend in different decades in nearly 50 years. It continued to increase from the 1960s to the 1990s. It increased most greatly from the 1970s to the 1980s but decreased slightly from the 1990s to the 2000s.展开更多
The native and introduced ground cover plants were screened by field survey,cultivation test and configuration effect evaluation in arid valleys of Ganzi Tibetan area.A total of 205 species belonging to 140 genera,67 ...The native and introduced ground cover plants were screened by field survey,cultivation test and configuration effect evaluation in arid valleys of Ganzi Tibetan area.A total of 205 species belonging to 140 genera,67 families were selected as applicable types.Among them,there were 53 species of evergreen shrubs,36 species of deciduous shrubs,17 species of woody vines,99 species of herbaceous plants;27 species of color-leafed plants,8 species of succulent plants.And 79 species were recommended as the best ground cover plants.Higher plants in Ganzi Tibetan area were increased to 5,362 species,1147 genera,244 families through screening.展开更多
Through exploring current outdoor tourism development of Ganzi Prefecture and its tourism development prospects, this study planned the pertinent outdoor tourism product system according to its background advantages. ...Through exploring current outdoor tourism development of Ganzi Prefecture and its tourism development prospects, this study planned the pertinent outdoor tourism product system according to its background advantages. Outdoor tourism development of Ganzi Prefecture helps to promote the development of its all-for-one tourism, enrich categories of local tourism products, enhance rural transformation and poverty-alleviation tourism development, and promote the sustainability of local tourism industry.展开更多
文摘The Ganzi geothermal field is located in the Songpan-Ganzi orogenic belt in Sichuan Province.Many hot springs are exposed along the Yalahe valley in Ganzi geothermal field,which is a favorable area for hightemperature geothermal resource exploration.However,the geological model of heat exchange,the regional structure controlling hydrothermal convection and the development model of geothermal reservoirs are still unclear.Therefore,further studies are necessary to meet the geothermal exploration requirements in the middle and deep strata of this geothermal field.In this study,a geological model of the geothermal system of Ganzi geothermal field is proposed.We are convinced that there exists a hydrothermal convection system in the Ganzi geothermal field,the heat transfer of which is accomplished through deep-rooted major faults.Therefore,the identification of deep-rooted major faults and the description of geothermal reservoirs are the research objects of the integrated geophysical methods.The main factors controlling the geothermal reservoirs in the deep-rooted Xianshuihe major fault and Yalahe fault zones are analyzed by using gravity,aeromagnetic,and electromagnetic methods and techniques.The analysis results of regional gravity and aeromagnetic anomalies show that the Xianshuihe major fault has produced obvious gravity and aeromagnetic anomalies on the surface,and thus the position and strike of this fault can be accurately predicted by inversion of the aeromagnetic anomalies.Geothermal reservoirs show low-resistivity anomalies in the electromagnetic profile.The inversion results of the controlled source audio-frequency magnetotelluric(CSAMT)data show that geothermal reservoirs are mainly developed along the Yalahe valley,and the west side of the valley is more favorable for geothermal exploration.This study is of guiding significance to the efficient exploitation and utilization of the Ganzi geothermal field.
基金supported by the SINOPEC Exploration Southern Company(the National Oil and Gas Special Projects XQ-04)the Special Fund for Basic Scientific Research of Central Colleges, Chang'an University(CHD2011JC185)
文摘Major, trace and rare earth element （REE） concentrations of Late Triassic sediments （fine- grained sandstones and mudstones） from Hongcan Well 1 in the NE part of the Songpan-Ganzi Basin, western China, are used to reveal weathering, provenance and tectonic setting of inferred source areas. The Chemical Index of Alteration （CIA） reflects a low to moderate degree of chemical weathering in a cool and somewhat dry climate, and an A-CN-K plot suggests an older upper continental crust prove- nance dominated by felsic to intermediate igneous rocks of average tonalite composition. Based on the various geochemical tectonic setting discrimination diagrams, the Late Triassic sediments are inferred to have been deposited in a back-arc basin situated between an active continental margin （the Kunlun- Qinling Fold Belt） and a continental island arc （the Yidun Island Arc）. The Triassic sediments in the study area underwent a rapid erosion and burial in a proximal slope-basin environment by the petrographic data,while the published flow directions of Triassic turbidites in the Aba-Zoige region was not supported Yidun volcanic arc source. Therefore, we suggest that the Kunlun-Qinling terrane is most likely to have supplied source materials to the northeast part of the Songpan-Ganzi Basin during the Late Triassic.
基金Supported by the Project of Education Department of Sichuan Province,China(16ZB0365)Project of Sichuan Minzu College(XYZB18041SB)
文摘Based on the statistical data of daily precipitation in 14 meteorological stations of Ganzi Prefecture from 1960 to 2011, the temporal variation characteristics of precipitation in Ganzi Prefecture in nearly 50 years were studied. The results showed that in Ganzi Prefecture, annual precipitation showed an increasing trend, and averaged 659 mm in nearly 50 years, mainly varying from 550 to 750 mm. In a year, precipitation was mainly distributed in summer and autumn, and the precipitation in summer and autumn accounted for 83% of annual precipitation. Seen from the interdecadal variation of annual precipitation, annual precipitation in Ganzi Prefecture showed an increasing trend in different decades in nearly 50 years. It continued to increase from the 1960s to the 1990s. It increased most greatly from the 1970s to the 1980s but decreased slightly from the 1990s to the 2000s.
基金Sponsored by Scientific Research Project of State Ethnic Affairs Commission(14SCZ004)School-level Incubation Program of Sichuan Minzu College(KBFHA18004)Applied Demonstration Course of Sichuan Minzu College(sfkc201715).
文摘The native and introduced ground cover plants were screened by field survey,cultivation test and configuration effect evaluation in arid valleys of Ganzi Tibetan area.A total of 205 species belonging to 140 genera,67 families were selected as applicable types.Among them,there were 53 species of evergreen shrubs,36 species of deciduous shrubs,17 species of woody vines,99 species of herbaceous plants;27 species of color-leafed plants,8 species of succulent plants.And 79 species were recommended as the best ground cover plants.Higher plants in Ganzi Tibetan area were increased to 5,362 species,1147 genera,244 families through screening.
基金Sponsored by Project of Sichuan Minzu College(YZB18041SB)。
文摘Through exploring current outdoor tourism development of Ganzi Prefecture and its tourism development prospects, this study planned the pertinent outdoor tourism product system according to its background advantages. Outdoor tourism development of Ganzi Prefecture helps to promote the development of its all-for-one tourism, enrich categories of local tourism products, enhance rural transformation and poverty-alleviation tourism development, and promote the sustainability of local tourism industry.
