Changes in physical features of Glacier No. 1 of the Tianshan Mountains in response to climate change

This study analyzes the changes in glacier zones and snow composition of Glacier No.1 in the Tianshan Mountains of China since 1961,and their possible relations with climate.It is found that precipitation dominated the snow composition and that air temperature and precipitation controlled the distribution of glacier zones,but interannual change in precipitation had a relatively large effect on glacier zones and snow composition during 1963–1981 (P10) and 1963–1989 (P11).However,during 1982–2007 (P20) and 19...     

皖南山区环境地质特征与滑坡地质灾害防治

文章以皖南山区环境地质特征、岩土体组成及其工程性质研究为基础,从人类工程活动与地质环境的互馈作用分析入手,探讨区域环境工程地质作用规律,对滑坡等地质灾害的发生及发展趋势进行预测;研究表明,对地质生态环境防护和塑造人地和谐的人类生存环境及保证区域经济、社会和环境可持续发展战略具有重要意义。     

天山大峡谷国家森林公园土地利用变化及生态系统服务价值研究

通过对1990年、2000年、2010年和2018年4期遥感解译的土地利用数据,采用土地利用动态度、生态系统服务价值评价和敏感性分析等方法,分析了研究区的土地利用变化及生态系统服务功能,同时以ArcGIS软件为支撑,探讨了天山大峡谷国家森林公园在不同时期内的土地利用变化对生态系统服务(ESV)的影响.研究结果表明:19...     

浅论江南丘陵城市环境特色的传承与发扬——以吉安市中心城市为例

针对当前快速发展的城市化进程中普遍存在的城市特色丧失的状况，阐述城市所处地域环境的唯一性是城市特色构成的关键元素。在归纳我国江南丘陵地带城市普遍具备的自然环境优势，并分析其对城市特色所起的作用后，结合吉安市的具体情况，提出了丘陵地带城市特色的传承与发扬的系列思考，包括城市腹地范围山水特色整体风貌与人文景观遗存的保护和利用；城区外围近郊背景圈中农村居民点规划和产业结构的调整；城区边缘城郊结合部的规划引导；城市片区之间的衔接过渡；城市街区环境特色创造以及具体的城市建设项目的实施等六个层面。     

Factors influencing anuran distribution in coastal dune wetlands in southern Brazil

We investigated the potential role of hydroperiod and habitat structural complexity as explanatory factors defining richness, abundance and spatial and temporal distribution of anurans in wetlands of coastal dunes. This survey was performed in 15 wetlands along the Atlantic coastal zone of southern Brazil. We identified 10 anuran species (nine in the adult and eight in the tadpole stage) distributed in seven genera from five families. The adult richness and abundance varied among the hydroperiod classes, but without temporal variations. Both tadpole richness and abundance varied temporally and both were influenced by hydroperiod. Adult anuran composition was associated with dry months and wetland area, whereas tadpole composition was associated with emergent and floating macrophytes, wetland area and vegetation cover. This study identified the importance of habitat structural complexity and hydroperiod in spatial–temporal distribution models of anurans.     

东天山造山带区域变质作用及其构造环境研究

以活动论思想为指导，分析了东天山造山带区域变质作用的基本特征，成因类型，变质岩分带特征和特征矿和的组合的空间分规律，论证了大型断裂构造对区域变作用的同期制约和后期迭加改造作用，阐明了断裂区域变质作用在东天山普遍性以及断裂活动与变质变形，混合容化和花岗岩化作用之间的关系。最后对东天山变质岩带的板块构造环境和多期变质演化规律进行了探讨。     

Radiolarian record to paleoecological environment change events over the past 1.2 MaBP in the southern South China Sea

This note studies the Radiolarian fossil groups since 1.2 MaBP in ODP leg 184 site 1143, the southern South China Sea (SCS). The result shows that radiolarian abundance experienced a significant variation: before 0.9 MaBP it remained at the extremely low level, but increased with low extent between 0.9–0.65 Ma, which corresponded to the Mid-Pleistocene Transition stage, and it increased rapidly after 0.65 MaBP. During the whole process, the average abundance became higher and higher in each stage, and showed regularly periodic fluctuations. The obvious increase after 0.65 MaBP is inferred to result from the enhanced upwelling in this region, which was induced by the intensified monsoon circulation after the “Mid-Pleistocene Transition”. An outstanding result of the spectral analyses is that a long oscillation of ∼ 0.2 Ma cycle was found in the records of radiolarian abundance and complex diversity, which corresponds well to the result of other paleoceanographic indexes. This probably indicated a special cycle characteristic of paleoecological environment evolution in this area. In addition, all of the radiolarian indexes show an obvious boundary in about 0.47 MaBP, indicating the abrupt variation of the community structure and radiolarian abundance level before and after 0.47 MaBP. So we suppose that there existed a distinct change event of oceanic ecology environment during that period.     

南戏传奇化与传奇昆曲化

明代戏曲体制的演变,如果说是从南戏传奇化揭开序幕的话,则标志着这种演变最终完成的便是传奇昆曲化。换句话说,只有到了这一步,明代戏曲才能得以展示一种比较完整的艺术面貌。     

Geochemical characteristics and tectonic implications of HP-UHP eclogites and blueschists in southwestern Tianshan, China

Four rock assemblages in correspondence with two different tectonic settings have been recognized in the NEE-SWW extending HP-UHP metamorphic belt in southwestern Tianshan, northwest China. Eclogite assemblage EC1 is geochemically akin to alkaline within-plate oceanic island basalt (OIB). EC2 shows affinity to enriched mid-oceanic ridge basalt (EMORB). Rare earth element (REE) and other immobile trace element characteristics of blueschist assemblage BS1 resemble those of normal mid-oceanic ridge basalt (NMORB). These three assemblages are likely formed on a seamount setting, and the prevalent presence of carbonate minerals and omphacite quartzite stripes/gobbets suggests ancient pelagic sediments including marls are probably developed upon the basaltic seamount. Whereas the geochemical characteristics of BS2 assemblage are of volcanic arc basalt-type. The seamount with the pelagic sediments on it is brought into the subduction zone, and volcanic arc basalts formed on the active continental margin and trench sediments are eroded and enwrapped in the subducting mass, they are altogether subjected to high to ultrahigh pressure metamorphism and subsequent exhumation towards surface. The HP-UHP metamorphic belt is thus interpreted as a subduction-accretionary complex formed by tectonic juxtaposition and imbrication of seamount, seafloor, trench and volcanic arc sequences during oceanic crust subduction.     

新疆西天山西段金铜成矿带——中亚成矿域东延

新疆西天山西段位于哈萨克斯坦 -伊犁板块的东南部边缘 ,包括伊犁石炭纪裂谷、那拉提地块、哈尔克早古生代被动陆缘褶皱带。主要已知矿床 (点 )按其容矿围岩可分为镁铁 -超镁铁岩型、斑岩型、花岗岩型、矽卡岩型、陆相火山岩型、陆相沉积岩型、浅变质含碳碎屑岩型。根据区内成矿地质条件、矿化特征 ,区内以找金矿主 ,兼顾铜镍矿等。金矿以穆龙套型和火山岩型金矿为主 ,同时注意卡林型和中 -酸性侵入岩内外接触带型 ;铜矿以镁铁 -超镁铁岩型和火山岩型为主。地质与成矿条件与中亚成矿域具有可比性 ,因此 ,新疆西天山西段金铜成矿带应为中亚成矿域东延部分