The recently identified Huashan ophiolitic mélange was considered as the eastern part of the Mianlüe suture in the Qinling orogenic belt. SHRIMP zircon U-Pb geochronology on gabbro from the Huashan ophiolite...The recently identified Huashan ophiolitic mélange was considered as the eastern part of the Mianlüe suture in the Qinling orogenic belt. SHRIMP zircon U-Pb geochronology on gabbro from the Huashan ophiolite and granite intruding basic volcanic rocks indicates crystallization ages of 947±14 Ma and 876±17 Ma respectively. These ages do not support a recently proposed Hercynian Huashan Ocean, but rather favor that a Neoproterozoic suture assemblage （ophiolite） is incorporated into the younger （Phanerozoic） Qinling orogenic belt.展开更多
Huashan pine (Finus armandii Franch) is a poential species for dendroclimatic study. Ring-width cores were sampled for four stands of two sites from the eastern extreme of the Qinling Mountains. The ring-width chronol...Huashan pine (Finus armandii Franch) is a poential species for dendroclimatic study. Ring-width cores were sampled for four stands of two sites from the eastern extreme of the Qinling Mountains. The ring-width chronologies developed in this study cover a maximum Period from A.D. 1359 t0 1992 and show high common chronology variance over the common period 1911-1960.All the chronologies are significantly correlated with all others, and the degree of correlation appears related to tree age. Response function analyses reveal that from 41 to 75 Percent of chronology variance can be accounted for by monthly mean air temperature and monthly total precipitation. A sufficiently strong correlation of ringwidth index with May and June rainfall and June temperature exists, implying soil moisture to be a limiting factor for Huashan pine growth. The association displayed by response diagrams between narrow rings, low precipitation, and high temperature during spring and early summer indicates a promising potential of ring widths for reconstruction of spring drought for the study area.展开更多
The Weihe Graben is not only an important Cenozoic fault basin in China but also a significant active seismic zone. The Huashan piedmont fault is an important active fault on the southeast side of the Weihe Graben and...The Weihe Graben is not only an important Cenozoic fault basin in China but also a significant active seismic zone. The Huashan piedmont fault is an important active fault on the southeast side of the Weihe Graben and has been highly active since the Cenozoic. The well–known Great Huaxian County Earthquake of 1556 occurred on the Huashan piedmont fault. This earthquake, which claimed the lives of approximately 830000 people, is one of the few large earthquakes known to have occurred on a high–angle normal fault. The Huashan piedmont fault is a typical active normal fault that can be used to study tectonic activity and the associated hazards. In this study, the types and characteristics of late Quaternary deformation along this fault are discussed from geological investigations, historical research and comprehensive analysis. On the basis of its characteristics and activity, the fault can be divided into three sections, namely eastern, central and western. The eastern and western sections display normal slip. Intense deformation has occurred along the two sections during the Quaternary; however, no deformation has occurred during the Holocene. The central section has experienced significant high–angle normal fault activity during the Quaternary, including the Holocene. Holocene alluvial fans and loess cut by the fault have been identified at the mouths of many stream valleys of the Huashan Mountains along the central section of the Huashan piedmont fault zone. Of the three sections of the Huashan piedmont fault, the central section is the most active and was very active during the late Quaternary. The rate of normal dip–slip was 1.67–2.71±0.11 mm/a in the Holocene and 0.61±0.15 mm/a during the Mid–Late Pleistocene. As is typical of normal faults, the late Quaternary activity of the Huashan piedmont fault has produced a set of disasters, which include frequent earthquakes, collapses, landslides, mudslides and ground fissures. Ground fissures mainly occur on the hanging–wall of the Huashan piedmont fault, with landslides, collapses and mudslides occurring on the footwall.展开更多
Systematical Sr, Nd and O isotopic studies were made on the Huashan granite complex in Guangxi. Incombination with the studies of geological, petrological and geochemical data, it is believed that the complexconsists ...Systematical Sr, Nd and O isotopic studies were made on the Huashan granite complex in Guangxi. Incombination with the studies of geological, petrological and geochemical data, it is believed that the complexconsists of granites of three stages. with different geneses and different source materials. They are not the prod-ucts of differentiation and evolution of one single consanguineous magma. Granites of the 1st stage are of theIndosinian syntectic type or I type, also derived from a mixed mantle-crustal source. Those of the 2nd stage areof the early Yanshanian syntectic type or I type. also derived from a mixed mantle-crustal source, and those ofthe 3rd stage are of the late Yanshanian transformed type or S type. derived from a crustal source.展开更多
On the basis of field observation and measuring data, the authors discuss the types,distributing regularity and gemesos of geological disasters on the Northern Huashan predmont and its foreland plain. We think that ...On the basis of field observation and measuring data, the authors discuss the types,distributing regularity and gemesos of geological disasters on the Northern Huashan predmont and its foreland plain. We think that the activity of Northern Huashan piedmont fault zone since Quaternary period makes the mountain highly uplift,which provide a favorable terrain condition for gravitatiotal geological hazard;the recent activity of the buried fault on the foreland plain is the main reason of ground cracking and sinking .Finally ,we make a synthetical analysis of geological hazard risk on the study area.展开更多
In this paper, CVM method (conditional value evaluation method, also known as willingness investigation method) is used to investigate the willingness to pay about the ecological environment protection cost of Shaanxi...In this paper, CVM method (conditional value evaluation method, also known as willingness investigation method) is used to investigate the willingness to pay about the ecological environment protection cost of Shaanxi Huashan scenic spot in July and August, 2013. By establishing the Logistic regression model, the per capita willingness to pay (WTP) of the tourists is calculated to be 79.2 yuan / person. The results show that the tourists' awareness of environmental protection is increasing day by day, and the visitors are fully aware of the importance of protecting the ecological environment. 57.85% of the tourists will be willing to pay, including civil servants, self-employed persons, college degree or above, family monthly income in the 8000-10000 yuan visitors will pay higher. This provides a reference for the sustainable development and development of ecotourism in Huashan Scenic Spot.展开更多
Huashan Rock Art(HRA) has increasingly drawn nationwide and even worldwide attention as scholars have completed and published multidisciplinary studies of the art, thus promoting a positive impact on the local tourism...Huashan Rock Art(HRA) has increasingly drawn nationwide and even worldwide attention as scholars have completed and published multidisciplinary studies of the art, thus promoting a positive impact on the local tourism and economy.Through on-the-spot observations and in-depth interviews with local officials, farmers, and visiting tourists, this paper presents the cultural landscape of the HRA area from the perspectives of "place" and "space," which have been little explored in previous studies of the HRA area.Presently, both the natural and cultural landscape of Huashan have been restructured by the local government and inscribed on the World Heritage List, and the problems of sustainable preservation of the rock art, balancing dynamic development with expanded tourism, and conserving the cultural heritage of the HRA are being addressed.展开更多
Huashan rock painting is a representative of the rock art complex in Zuojiang River in Guangxi Zhuang Autonomous Region,and it is the largest and the most well preserved rock painting found in China,with a wide distri...Huashan rock painting is a representative of the rock art complex in Zuojiang River in Guangxi Zhuang Autonomous Region,and it is the largest and the most well preserved rock painting found in China,with a wide distribution of locations and the richest content of images.Due to its grand scale,spectacular scenes,and numerous images,it has become a typical representative of rock painting in Zuojiang River basin of Guangxi and is famous all over the world.In 1988,it was announced as a key cultural relics protection unit by the State Council,and in 2016,“Zuojiang River Huashan Rock Art Cultural Landscape”was successfully applied for the List of World Heritage,which makes it important to the inheritance and protection of Huashan rock paintings.In the past 10 years,with the successful holding of China-ASEAN Expo,the distinctive tourist products of Guangxi Zhuang nationality and the culture creative product industry have been vigorously developed and recognized by domestic and foreign markets.The culture of Guangxi Zuojiang Huashan rock painting can be presented in the form of cultural and creative products,so that Guangxi Zuojiang River Huashan rock art can be known by more people.展开更多
基金the National Natural Science Foundation of China （Grant No. 40234045, 40473030）.
文摘The recently identified Huashan ophiolitic mélange was considered as the eastern part of the Mianlüe suture in the Qinling orogenic belt. SHRIMP zircon U-Pb geochronology on gabbro from the Huashan ophiolite and granite intruding basic volcanic rocks indicates crystallization ages of 947±14 Ma and 876±17 Ma respectively. These ages do not support a recently proposed Hercynian Huashan Ocean, but rather favor that a Neoproterozoic suture assemblage （ophiolite） is incorporated into the younger （Phanerozoic） Qinling orogenic belt.
文摘Huashan pine (Finus armandii Franch) is a poential species for dendroclimatic study. Ring-width cores were sampled for four stands of two sites from the eastern extreme of the Qinling Mountains. The ring-width chronologies developed in this study cover a maximum Period from A.D. 1359 t0 1992 and show high common chronology variance over the common period 1911-1960.All the chronologies are significantly correlated with all others, and the degree of correlation appears related to tree age. Response function analyses reveal that from 41 to 75 Percent of chronology variance can be accounted for by monthly mean air temperature and monthly total precipitation. A sufficiently strong correlation of ringwidth index with May and June rainfall and June temperature exists, implying soil moisture to be a limiting factor for Huashan pine growth. The association displayed by response diagrams between narrow rings, low precipitation, and high temperature during spring and early summer indicates a promising potential of ring widths for reconstruction of spring drought for the study area.
基金granted by the Geological Investigation Project of China Geological Survey (Grant Nos.1212011120102 and 12120115003501)
文摘The Weihe Graben is not only an important Cenozoic fault basin in China but also a significant active seismic zone. The Huashan piedmont fault is an important active fault on the southeast side of the Weihe Graben and has been highly active since the Cenozoic. The well–known Great Huaxian County Earthquake of 1556 occurred on the Huashan piedmont fault. This earthquake, which claimed the lives of approximately 830000 people, is one of the few large earthquakes known to have occurred on a high–angle normal fault. The Huashan piedmont fault is a typical active normal fault that can be used to study tectonic activity and the associated hazards. In this study, the types and characteristics of late Quaternary deformation along this fault are discussed from geological investigations, historical research and comprehensive analysis. On the basis of its characteristics and activity, the fault can be divided into three sections, namely eastern, central and western. The eastern and western sections display normal slip. Intense deformation has occurred along the two sections during the Quaternary; however, no deformation has occurred during the Holocene. The central section has experienced significant high–angle normal fault activity during the Quaternary, including the Holocene. Holocene alluvial fans and loess cut by the fault have been identified at the mouths of many stream valleys of the Huashan Mountains along the central section of the Huashan piedmont fault zone. Of the three sections of the Huashan piedmont fault, the central section is the most active and was very active during the late Quaternary. The rate of normal dip–slip was 1.67–2.71±0.11 mm/a in the Holocene and 0.61±0.15 mm/a during the Mid–Late Pleistocene. As is typical of normal faults, the late Quaternary activity of the Huashan piedmont fault has produced a set of disasters, which include frequent earthquakes, collapses, landslides, mudslides and ground fissures. Ground fissures mainly occur on the hanging–wall of the Huashan piedmont fault, with landslides, collapses and mudslides occurring on the footwall.
基金supported by the National Natural Science Foundation of China
文摘Systematical Sr, Nd and O isotopic studies were made on the Huashan granite complex in Guangxi. Incombination with the studies of geological, petrological and geochemical data, it is believed that the complexconsists of granites of three stages. with different geneses and different source materials. They are not the prod-ucts of differentiation and evolution of one single consanguineous magma. Granites of the 1st stage are of theIndosinian syntectic type or I type, also derived from a mixed mantle-crustal source. Those of the 2nd stage areof the early Yanshanian syntectic type or I type. also derived from a mixed mantle-crustal source, and those ofthe 3rd stage are of the late Yanshanian transformed type or S type. derived from a crustal source.
文摘On the basis of field observation and measuring data, the authors discuss the types,distributing regularity and gemesos of geological disasters on the Northern Huashan predmont and its foreland plain. We think that the activity of Northern Huashan piedmont fault zone since Quaternary period makes the mountain highly uplift,which provide a favorable terrain condition for gravitatiotal geological hazard;the recent activity of the buried fault on the foreland plain is the main reason of ground cracking and sinking .Finally ,we make a synthetical analysis of geological hazard risk on the study area.
文摘In this paper, CVM method (conditional value evaluation method, also known as willingness investigation method) is used to investigate the willingness to pay about the ecological environment protection cost of Shaanxi Huashan scenic spot in July and August, 2013. By establishing the Logistic regression model, the per capita willingness to pay (WTP) of the tourists is calculated to be 79.2 yuan / person. The results show that the tourists' awareness of environmental protection is increasing day by day, and the visitors are fully aware of the importance of protecting the ecological environment. 57.85% of the tourists will be willing to pay, including civil servants, self-employed persons, college degree or above, family monthly income in the 8000-10000 yuan visitors will pay higher. This provides a reference for the sustainable development and development of ecotourism in Huashan Scenic Spot.
文摘Huashan Rock Art(HRA) has increasingly drawn nationwide and even worldwide attention as scholars have completed and published multidisciplinary studies of the art, thus promoting a positive impact on the local tourism and economy.Through on-the-spot observations and in-depth interviews with local officials, farmers, and visiting tourists, this paper presents the cultural landscape of the HRA area from the perspectives of "place" and "space," which have been little explored in previous studies of the HRA area.Presently, both the natural and cultural landscape of Huashan have been restructured by the local government and inscribed on the World Heritage List, and the problems of sustainable preservation of the rock art, balancing dynamic development with expanded tourism, and conserving the cultural heritage of the HRA are being addressed.
基金This paper is the promotion project of basic ability of scientific research of young and middle-aged teachers in Guangxi universities-the phase research result of Application and Research of Huashan Rock Paintings in Cultural and Creative Products,with the project No.of 2019KY0891.
文摘Huashan rock painting is a representative of the rock art complex in Zuojiang River in Guangxi Zhuang Autonomous Region,and it is the largest and the most well preserved rock painting found in China,with a wide distribution of locations and the richest content of images.Due to its grand scale,spectacular scenes,and numerous images,it has become a typical representative of rock painting in Zuojiang River basin of Guangxi and is famous all over the world.In 1988,it was announced as a key cultural relics protection unit by the State Council,and in 2016,“Zuojiang River Huashan Rock Art Cultural Landscape”was successfully applied for the List of World Heritage,which makes it important to the inheritance and protection of Huashan rock paintings.In the past 10 years,with the successful holding of China-ASEAN Expo,the distinctive tourist products of Guangxi Zhuang nationality and the culture creative product industry have been vigorously developed and recognized by domestic and foreign markets.The culture of Guangxi Zuojiang Huashan rock painting can be presented in the form of cultural and creative products,so that Guangxi Zuojiang River Huashan rock art can be known by more people.
