The geological characteristics of oceanic-type UHP metamorphic belts and their tectonic implications: Case studies from Southwest Tianshan and North Qaidam in NW China

The geological characteristics of ultrahigh-pressure （UHP） metamorphic belts formed by deep subduction of oceanic crust are summarized in this paper. Oceanic-type UHP metamorphic belt is characterized by its protolithlc assemblage of typical oceanic crust, the peak metamorphic temperature 〈600℃, P-T path undergoing blueschist facies during prograde and retrograde metamorphic evolution, reepectively, with low geothermal gradient of cold subduction. The further study of oceanic-type UHP metamorphic belt is very significant for constructing metamorphic reaction series of cold subduction zone, for understanding how aqueous fluids were transported into deep mantle and for classifying the types of UHP metamorphism in cold subduction zone. The uplift and exhumation mechanism of oceanic UHP metamorphic rocks is one of the most challenging problems in the study of UHP metamorphism, which is very important for understanding the geodynamic mechanism of solid Earth. As a traveler eubducted into the mantle depth end then uplifted to the surface, oceanic-type UHP metamorphic belts witness the bulk process from the subduction to exhumation and is an ideal target to study the geochemical behavior end cycling of elements in subduction zones. The tectonic evolution of one convergent orogenic belt can be usually divided into two stages of oceanic subduction and followed continental subduction and collision, and the two best-established examples of orogenic belts are Alpa and Himalaya. Therefore, the study of oceanic-type UHP metamorphic belt is the frontier of the current plate tectonic theory. As two case studies, the current status and existing problems of oceanic-type UHP metamorphic belts in Southwest Tianshan and North Qaidam, NW China, are reviewed in this paper.     

The northern annular mode: More zonal symmetric than the southern annular mode

Fan （2007） recently documented the zonal asymmetry of the Antarctic oscillation （AAO） in the austral winter. In this research, the zonal asymmetry of the northern annular mode, or the Arctic oscillation （AO）, in the interannual variability is studied for the boreal winter. It is shown that there is zonal asymmetry of the AO as well, similar to the case of the Antarctic oscillation （AAO）. However, the zonal asymmetry of the AO is considerably weaker than that of the AAO. This is far beyond the speculation, since the zonal asymmetry of the geography is larger in the Northern Hemisphere than the Southern Hemisphere. The Western and Eastern Hemispheres portions of the AO are correlated at 0.54 for 1959-1998, comparing with 0.23 for the case of the AAO. The authors also discussed the physical reason for this inter-hemispheric difference, and partly attributed it to the El Ni~o and Southern Oscillation （ENSO） cycle which may be represented by the SO index. It is indicated that the SO associated sea-level pressure （SLP） patterns are more zonal symmetric in the high latitudes of the Northern Hemisphere than the Southern Hemisphere.     

川南地区下古生界海相页岩微观储集空间类型

为探明不同成因的孔隙对页岩气储集的贡献,基于多种分析测试手段,对川南地区下古生界海相页岩微孔类型与分布、孔隙定量表征进行研究,并探讨页岩中微观储集空间的成因及影响因素。结果表明:下古生界页岩微观储集空间分为矿物基质孔、有机孔和微裂缝3大类,并可进一步细分为9种类型;龙马溪组页岩主要发育有机质孔和黏土矿物层间孔,五峰组页岩主要发育有机质孔和溶蚀孔、缝,九老洞组页岩有机质孔极少,多见溶蚀孔、缝;下古生界3套页岩孔隙类型与分布特征的差异与矿物组成、有机质丰度和成岩演化作用有关;龙马溪组底部页岩微孔发育,比表面积大,为页岩气的吸附提供大量储集空间,是有利的页岩储层发育段。     

新疆东天山地区自然铜矿带地质特征

文章对新疆东天山自然铜成矿带的地质特征进行了研究,该自然铜矿化带处于觉罗塔格金、铜、铁构造成矿带内,自然铜矿点自西向东分布于十里坡地区、黑龙峰地区和长城山地区;自然铜矿点的赋矿围岩为下石炭统马头滩组玄武岩和凝灰岩,矿石矿物主要以自然铜和砷铜矿为主,自然铜矿点中铜含量较高;通过对十里坡和黑龙峰自然铜矿点2个地球化学剖面的研究和对比,表明成矿元素铜受地层控制明显,2个自然铜矿点在大地构造位置,赋矿地层,赋矿岩石、铜的赋存状态和成矿元素组合方面有很多共性,认为东天山若干自然铜矿点是同一成矿作用的产物,东天山地区可能存在连续几百公里的自然铜成矿带.     

闽南地区民企人力资源管理中的问题及对策

改革开放后,闽南地区民营企业发展迅猛,为闽南地区经济的发展,人民生活水平的提高做出巨大贡献,在福建省经济发展中具有举足轻重的地位。但是。普遍存在的人力资源管理理念落后、管理方式陈旧、管理水平偏低等现象．严重地制约了企业的发展。本文就该地区民营企业人力资源管理中存在的问题进行深入的分析,在此基础上提出相应的具有实用性的对策建议．并对如何加强闽南地区民营企业人力资源管理作出进一步思考。     

近代闽南侨乡“五脚基”与“洋楼”表征关系解析

基于皮尔斯的符号三角理论和实证分析,提出在近代闽南侨乡文化的特殊场合下,"五脚基"能成为"洋楼"的表征符号的观点."五脚基"作为一种符号媒介,能够与"洋楼"客体对象建立表征关系,这种表征关系体现为存在关联、标识关联、类构关联3个方面,而"五脚基"符号媒介在与"洋楼"客体对象建立表征关系后,它也就能上升为一种更"发达"的符号."五脚基"除了作为闽南人用来指代"外廊文化体"的符号外,当其处在近代闽南侨乡特定的文化场合内的时候,却还有表征"洋楼"的功能.     

“2010.12.11”云南冬季暴雨成因分析

 应用常规观测资料、FY-2C卫星云图和NCEP再分析资料,通过诊断分析研究了2010年12月11日发生在滇中及以南地区的云南暴雨天气过程.结果发现,这次冬季暴雨天气过程发生在有利的环流背景下,ITCZ位置偏北较活跃,孟湾存在大片对流云系,中印度洋10°N附近存在一支异常的大尺度西南气流,孟加拉湾低层有一个热带气旋生成,在卫星云图上表现出明显的气旋式云系,孟湾热带气旋和90°E附近的南支槽及槽前西南低空急流东移造成了这次暴雨天气过程;引发暴雨的水汽和能量由低空急流从孟加拉湾输送而来,充沛的水汽在云南上空强烈辐合,暴雨区θ_se呈陡立状,暴雨发生在低层辐合高层辐散的上升运动区,水汽通量散度辐合区和湿Q矢量辐合区与暴雨区对应较好.     

试论闽南民间舞蹈中动作语言的创作特点

闽南民间舞蹈历史悠久,博大精深,颇具特色,是中国民族民间舞的一朵奇葩。本文通过研究闽南民间舞蹈为素材的创作作品,从准确性、生动性、独特性、文化性等方面解读分析闽南民间舞蹈动作语言的创作特点。     

伊犁盆地南缘乌库尔其铀矿床西山窑组下段砂体特征与铀成矿关系

通过对研究区中侏罗统西山窑组下段砂体厚度和砂地比特征进行分析,结合室内普通薄片镜下鉴定,在此基础上绘制了乌库尔其铀矿床西山窑组下段沉积相展布图,探讨了砂体对铀成矿的控制与影响,指出了砂体连通性和均质性变化部位,为铀成矿的有利部位;同时认为扇三角洲前缘水下分流河道砂体及一些平原分流河道砂体是赋存可地浸砂岩型铀矿的有利围岩。     

北美海棠6品种在南方地区的引种研究

【目的】探索北美海棠在南方地区的适应性和观赏性,为有效引种和培育新品种提供理论依据。【方法】以6个新优北美海棠品种(‘黛玉’、‘白兰地’、‘丰盛’、‘王族’、‘草莓果冻’和‘紫宝石’)为引种试材,在南方地区进行物候期、观赏性及耐热性观测和试验。【结果】6个北美海棠品种均能正常萌芽、展叶、开花、结果,且具有较高的观赏价值。夏季生长适应性观测显示,6个品种在南方高温环境下叶片出现不同程度的皱缩、卷曲、叶缘枯焦等变化。生理适应性表明,各品种均能通过自身质膜热稳定性、抗氧化系统及渗透调节方式应对南方夏季高温环境。【结论】6种北美海棠在南方地区夏季高温环境下生长受到一定影响,但通过自身的生理调节,能正常完成生活史,且表现出较高的观赏价值。引种的6种北美海棠表现最好的为‘黛玉’,其次是‘白兰地’和‘紫宝石’。南方地区可根据需要在苗木生产和景观绿化中选择适宜的北美海棠品种栽培。