Wuji Town,which is located by the east of Mt.Hengshan(one of the Five Mountains in China),and the side of Mishui River(a principal east-west water transport in ancient central and southern regions of Hunan),once was a...Wuji Town,which is located by the east of Mt.Hengshan(one of the Five Mountains in China),and the side of Mishui River(a principal east-west water transport in ancient central and southern regions of Hunan),once was an important commercial town and a political,economic and cultural center in the lower and middle reaches of Mishui River due to the particular historical opportunities.Its tourist resources are characterized by "integrated natural scenery and ancient town,highly concentrated scenic spots,prosperous business in the history,row upon row of stores and workshops,numerous temples and ancestral halls,and various festivals".It was proposed that the protection and rural tourism development of Wuji Town should be based on consciousness raising,unification of concepts,scientific planning,application of integrated protection means,and development of regional clusters on the basis of famous mountain and city.展开更多
The typical style and features of mountains and waters in Caoshi Ancient Town,have hitherto been well preserved. Caoshi Ancient Town boasts superior base of the natural eco-environment and deep-rooted background of re...The typical style and features of mountains and waters in Caoshi Ancient Town,have hitherto been well preserved. Caoshi Ancient Town boasts superior base of the natural eco-environment and deep-rooted background of regional culture,where mountains,waters,shoals,towns and other landscape elements are merged harmoniously,the transportation and geographical conditions have been fundamentally changed. Ancient towns,old temples,ancient forests,ancient wells and ancient piers are unique in different ways,with characteristics of tourism resources such as long history and ancient folklore. It should seize the historical opportunity of China vigorously developing rural tourism based on the construction of the new socialist countryside,to make characteristic agricultural economy gain ground; assume the leading role to drive the development of tourism economy in surrounding areas; correctly handle the relationship between development and protection to walk the path of sustainable development of tourism.展开更多
世界上典型热液脉型钴矿床,如五元素(Ag-Bi-Co-Ni-As±U)矿床,因其高的钴品位(高达8%)而具有重要的经济价值和研究意义,该类矿床以自然元素和砷化物组合为特征。不同于五元素矿床,湘东北横洞热液脉型钴矿床(中型,品位约0.04%)的矿...世界上典型热液脉型钴矿床,如五元素(Ag-Bi-Co-Ni-As±U)矿床,因其高的钴品位(高达8%)而具有重要的经济价值和研究意义,该类矿床以自然元素和砷化物组合为特征。不同于五元素矿床,湘东北横洞热液脉型钴矿床(中型,品位约0.04%)的矿石矿物组合为黄铁矿+黄铜矿+闪锌矿+方铅矿+磁黄铁矿,目前对该矿床中含钴矿物的特征及钴的富集机制尚不清楚。本文在详细的矿相学工作基础上,采用EPMA、EBSD、LA-ICPMS和LA-MC-ICPMS等多种分析方法,对其黄铁矿开展了精细结构、成分和硫同位素分析。将黄铁矿划分为PyI、PyII和PyIII三个世代。其中,PyII是Co的重要载体,常呈丝带状、不规则状或韵律环带交代PyI或呈细粒状产出,其Co含量高达52141×10^(-6),明显高于其他世代黄铁矿。黄铁矿中Co与Fe具有较好的负相关性,表明Co主要呈类质同象的形式置换Fe存于黄铁矿晶格中。而黄铁矿中高的Co/Ni比值(1.05~393)和Se含量(10.69×10^(-6)~129×10^(-6))则暗示了其热液成因。此外,PyII与PyI之间具有不规则港湾状接触界面、突变的化学成分以及相近的晶体取向,这些暗示了富钴的PyII系含钴流体与围岩及早阶段黄铁矿快速反应的产物,溶解再沉淀的动力学过程是控制PyII的形成机制。不同世代黄铁矿的δ34 S V-CDT值接近,变化范围为-13.12‰~-8.70‰,与围岩地层的硫同位素特征接近。结合湘东北结晶基底高的Co含量(30.4×10^(-6)~72.3×10^(-6))和以往流体包裹体显微测温结果,认为在晚侏罗世-早白垩世期间,NE-ENE向的长沙-平江断裂带走滑剪切活动使得深源热液流体从结晶基底连云山岩群活化萃取了金属钴,富钴热液沿走滑断裂向上运移至成矿部位,再因压力周期性变化引起流体发生不混溶作用进而分离,导致钴金属络合物失稳,最后钴沉淀富集成矿。通过与世界上典型热液脉型钴矿床成矿特征的对比,提出流体低的盐度和低砷、高硫的特征是造成横洞钴矿床矿物组合简单的主要控制因素。展开更多
基金Supported by Major Social Science Bidding Project of Hunan Province (2010ZDA10)Key Social Science Planning Project of Hengyang City(2010B009)+4 种基金Provincial-level Competitive Course Construction Project of Hunan Universities and Colleges[No33(2006)]Social Science Planning Project of Hengyang City(2009D19)Scientific Foundation of Hengyang Normal University(08C01)Foundation of Key Social Science Research Base of Hengyang CityKey Disciplinary Program of Tourism Management at Hengyang Normal University~~
文摘Wuji Town,which is located by the east of Mt.Hengshan(one of the Five Mountains in China),and the side of Mishui River(a principal east-west water transport in ancient central and southern regions of Hunan),once was an important commercial town and a political,economic and cultural center in the lower and middle reaches of Mishui River due to the particular historical opportunities.Its tourist resources are characterized by "integrated natural scenery and ancient town,highly concentrated scenic spots,prosperous business in the history,row upon row of stores and workshops,numerous temples and ancestral halls,and various festivals".It was proposed that the protection and rural tourism development of Wuji Town should be based on consciousness raising,unification of concepts,scientific planning,application of integrated protection means,and development of regional clusters on the basis of famous mountain and city.
基金Supported by Hunan Social Science Planning Project (2011YBB-053)Hengyang Key Social Science Planning Project (2011B (F) 038,2011B (F) 039)Hengyang Key Social Science Planning Project (2010B009)
文摘The typical style and features of mountains and waters in Caoshi Ancient Town,have hitherto been well preserved. Caoshi Ancient Town boasts superior base of the natural eco-environment and deep-rooted background of regional culture,where mountains,waters,shoals,towns and other landscape elements are merged harmoniously,the transportation and geographical conditions have been fundamentally changed. Ancient towns,old temples,ancient forests,ancient wells and ancient piers are unique in different ways,with characteristics of tourism resources such as long history and ancient folklore. It should seize the historical opportunity of China vigorously developing rural tourism based on the construction of the new socialist countryside,to make characteristic agricultural economy gain ground; assume the leading role to drive the development of tourism economy in surrounding areas; correctly handle the relationship between development and protection to walk the path of sustainable development of tourism.
文摘世界上典型热液脉型钴矿床,如五元素(Ag-Bi-Co-Ni-As±U)矿床,因其高的钴品位(高达8%)而具有重要的经济价值和研究意义,该类矿床以自然元素和砷化物组合为特征。不同于五元素矿床,湘东北横洞热液脉型钴矿床(中型,品位约0.04%)的矿石矿物组合为黄铁矿+黄铜矿+闪锌矿+方铅矿+磁黄铁矿,目前对该矿床中含钴矿物的特征及钴的富集机制尚不清楚。本文在详细的矿相学工作基础上,采用EPMA、EBSD、LA-ICPMS和LA-MC-ICPMS等多种分析方法,对其黄铁矿开展了精细结构、成分和硫同位素分析。将黄铁矿划分为PyI、PyII和PyIII三个世代。其中,PyII是Co的重要载体,常呈丝带状、不规则状或韵律环带交代PyI或呈细粒状产出,其Co含量高达52141×10^(-6),明显高于其他世代黄铁矿。黄铁矿中Co与Fe具有较好的负相关性,表明Co主要呈类质同象的形式置换Fe存于黄铁矿晶格中。而黄铁矿中高的Co/Ni比值(1.05~393)和Se含量(10.69×10^(-6)~129×10^(-6))则暗示了其热液成因。此外,PyII与PyI之间具有不规则港湾状接触界面、突变的化学成分以及相近的晶体取向,这些暗示了富钴的PyII系含钴流体与围岩及早阶段黄铁矿快速反应的产物,溶解再沉淀的动力学过程是控制PyII的形成机制。不同世代黄铁矿的δ34 S V-CDT值接近,变化范围为-13.12‰~-8.70‰,与围岩地层的硫同位素特征接近。结合湘东北结晶基底高的Co含量(30.4×10^(-6)~72.3×10^(-6))和以往流体包裹体显微测温结果,认为在晚侏罗世-早白垩世期间,NE-ENE向的长沙-平江断裂带走滑剪切活动使得深源热液流体从结晶基底连云山岩群活化萃取了金属钴,富钴热液沿走滑断裂向上运移至成矿部位,再因压力周期性变化引起流体发生不混溶作用进而分离,导致钴金属络合物失稳,最后钴沉淀富集成矿。通过与世界上典型热液脉型钴矿床成矿特征的对比,提出流体低的盐度和低砷、高硫的特征是造成横洞钴矿床矿物组合简单的主要控制因素。
