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Characteristics of geological structures in Shiling and Zhuanshanhu areas of Yehe Uplift,NE China
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作者 GUAN Yue YU Yinghua +1 位作者 ZHANG Yaxiong YUAN Hongqi 《Global Geology》 2024年第2期105-120,共16页
The basin marginal fault system is the key to understand the formation and evolution of Songliao Basin.In order to investigate the influence of marginal fault system on the structural evolution of Songliao Basin,a com... The basin marginal fault system is the key to understand the formation and evolution of Songliao Basin.In order to investigate the influence of marginal fault system on the structural evolution of Songliao Basin,a comprehensive study was conducted on Shiling Town and Zhuanshanhu area of Yehe Town in Siping City of Jilin Province,where is the southeastern margin of the Songliao Basin and there are a series of well-exposed fault,fold and intrusive bodies belonging to the main marginal fault system of the Songliao Basin known as the Jiamusi-Yitong(Jia-Yi)fault zone.Through profile measurement and field investigation,samples with various lithologies and distinctive features were collected.Detailed field and laboratory works include component and microstructure analysis of these samples,rock-rock contact analysis,main strike measurement and statistics analysis.These data reveal the structural characteristics of the fold,fault and intrusive bodies in the study area.The research results show that the folds are distributed in the Mesozoic strata near the main fault of the eastern branch of the Jia-Yi fault zone,and the folded strata involve the Cretaceous Denglouku and Quantou formations.In addition,the section is dominated by high-angle strikeslip thrust faults.Light-colored veins and dark-colored veins are extensively distributed in the exposed granites.Statistical analysis of joint and fault attitudes in the study area reveals a right-lateral strike-sliping along the main fault.The large-scale right-lateral strike-slip and thrust fault system in Shiling Town occurred in right-lateral transpressive stage in Late Cretaceous.Based on the results above,tectonic evolution sequence in Shiling section of the Jia-Yi fault zone during the Mesozoic can be divided into five stages:Middle Jurassic left-lateral ductile strike-slip stage,Late Jurassic compression stage,Early Cretaceous tension stage,Early Cretaceous extension stage and Late Cretaceous right-lateral transpressive stage.These may have important constraint on understanding the Mesozoic evolution of the Songliao Basin. 展开更多
关键词 Jia-Yi fault structural characteristics evolution sequence shiling Zhuanshanhu northern segment Tanlu fault
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Concept Planning of Ecological Landscapes on Urban Fringes——A Case Study of Landscape Concept Planning of Shiling Area in the Eastern New District of Chengdu City, Sichuan Province of China
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作者 廖春艳 沈一 《Journal of Landscape Research》 2011年第10期50-53,共4页
With Shiling Area of Eastern New District in Chengdu City as a background, concept design scheme was put forward from the perspective of ecological landscape through analyzing present development and ecological landsc... With Shiling Area of Eastern New District in Chengdu City as a background, concept design scheme was put forward from the perspective of ecological landscape through analyzing present development and ecological landscapes of the study area, applying philosophic thinking and Abstract concepts, and also combining with actual conditions of Chengdu, and meanwhile, concepts, orientation and functional structure of the eco-landscape concept planning were proposed. Key points of the planning were elaborated from 4 perspectives of spatial structure, traffic organization, spatial sequence and plant configuration to discuss spatial configuration of ecological landscapes on the fringes of Chengdu City, then further improve functions of ecological landscapes and quality of ecological environment, and put the concept planning into the construction practice of urban fringes. 展开更多
关键词 Urban FRINGES ECOLOGICAL landscapes shiling Area of Eastern New DISTRICT in Chengdu LANDSCAPE PLANNING
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河南省南召县石林沟铁多金属矿床地质特征和成因探讨 被引量:1
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作者 刘清泉 邵拥军 +2 位作者 刘忠法 郑明泓 徐桃 《南方金属》 CAS 2010年第1期28-30,共3页
分析了河南省南召县石林沟地区铁多金属矿床的地质特征及成因.矿床矿体呈层状、似层状,与围岩产状一致.矿石结构有半自形晶粒状结构和他形粒状结构,另有少量残余结构、镶嵌结构等;构造主要有块状构造、条带状构造、浸染状构造等.初步认... 分析了河南省南召县石林沟地区铁多金属矿床的地质特征及成因.矿床矿体呈层状、似层状,与围岩产状一致.矿石结构有半自形晶粒状结构和他形粒状结构,另有少量残余结构、镶嵌结构等;构造主要有块状构造、条带状构造、浸染状构造等.初步认为该矿床是沉积变质热液改造型铁等多金属矿床. 展开更多
关键词 河南省 石林沟 铁多金属矿 矿床地质 矿床成因
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