Petrogenesis of Aoyougou high-silica adakite in the North Qilian orogen, NW China: Evidence for decompression melting of oceanic slab

A trondhjemitic body occurs in the Aoyougou area,the western part of the North Qilian orogen.It is geochemically characterized by high SiO 2,Na 2 O (high Na/K),elevated Sr/Y and (La/Yb) N,positive Sr anomaly,relatively enriched large ion lithophile elements (LILEs) and light rare earth elements (LREEs),and depleted Nb,Ta,Ti,resembling the high-silica adakite.Zircon U-Pb SHRIMP dating yields a weighted mean age of 438±3 Ma.This age is significantly younger than eclogitization ages of 460-490 Ma in the North Qilian orogen,suggesting that formation of the adakite postdates the subduction of oceanic crust in association with closure of the ancient Qilian Ocean.Whole-rock Sr and Nd isotopic analyses give initial ratios of I Sr =0.7044 0.7047 and Nd (t)=3.0 4.1,indicating that they are derived from partial melting of the juvenile oceanic crust.In view of the tectonic evolution of the North Qilian orogen,the high-silica adakite was probably derived from decompression melting of the exhumed eclogite at the depth of ～60 km.     

老顶山国家森林公园根际土壤动物多样性初步研究

本文采用方框法调查了山西长治老顶山国家森林公园内油松林、侧柏林和草本植物根际土壤动物的多样性.结果表明,该森林公园内的土壤动物种类共计16类、381只,隶属3门10纲12目.其中膜翅目为优势类群,原尾目和弹尾目为稀有类群,直翅目幼虫、蜘蛛目、鞘翅目成虫及幼虫、双翅目成虫及幼虫、马陆目、等足目、石蜈蚣目、地蜈蚣目、后孔目、柄眼目和蜱螨目为常见类群.各种样地内常见土壤动物类群组成和占群落总体数量的比例呈现一定差异.土壤动物垂直分布有明显的表聚性.     

伏牛山森林土壤有机碳密度与环境因子的关联性分析

【目的】建立森林土壤有机碳(SOC)密度与环境因子之间的回归关系,为快速评估森林土壤有机碳密度的空间分布提供理论参考。【方法】在河南省伏牛山区玉皇顶和鸡角尖山体上,设置21块不同海拔、树种、地形等环境因子的典型样地,测定各样地不同深度土层的SOC密度,分析SOC密度与环境因子之间的回归关系,确定预测土壤有机碳密度的一般性因子。【结果】研究区0～40 cm深度的土壤有机碳密度变化范围为8.93～14.38 kg/m²,平均值为11.52 kg/m²。树种类型、山体间的SOC密度差异不显著,同一树种SOC密度与同一山体方位、坡度等地形因子回归关系显著; 所有样地SOC密度与树木密度、凋落物厚度和叶面积指数等植被因子回归关系显著,与地形因子回归关系不显著; SOC密度与植被因子间的回归关系可解释73.3%的针叶林地SOC密度的变异,76.7%的阔叶林地SOC密度变异,以及71.8%的研究区所有林地的SOC密度变异。【结论】同一山体同一树种SOC密度,可以用方位、坡度等地形因子来描述; 同一山体不同树种或不同山体不同树种林地的SOC密度,可以用植被因子来描述; 植被因子是土壤有机碳密度预测的一般性因子,可以通过遥感等手段快速评估复杂地形内土壤有机碳的空间分布。     

木札岭华山松树轮宽度年表的建立及其气候响应

研究秦岭东部地区树轮对气候因子的响应,为该区域森林资源管理及抚育更新提供数据,并为气候重建提供参考。     

近50年新疆天山山区主要气候要素变化

利用天山山区具有较好代表性的10个气象台站1960-2009年的历史气候资料,运用线性倾向估计对天山山区近50年来气候变化的主要特征进行了分析。结果表明:近50年来,天山山区能量供给因子中的最高、最低、平均温度温度均呈明显的上升趋势,而日照时数、温度日较差呈明显的下降趋势,云量的变化趋势不明显。空气动力因子风速的下降趋势显著;湿度因子中空气相对湿度略有下降趋势,而水汽压、降水量略有上升趋势。受此影响,近50年天山山区气候总体趋于干向湿发展的趋势,气候朝暖湿方向变化。     

包容性增长理念下的特困片区扶贫开发研究——以罗霄山片区炎陵县为例

集中连片特困地区扶贫攻坚被划为"十二五"规划期间的重要内容,而湖南省株洲市炎陵县是中部地区罗霄山连片特困地区的典型贫困县之一,贫困状况严峻。通过对炎陵县进行实地调查和数据统计分析,在炎陵县扶贫规划中应以包容性增长理念为指导,调整和优化产业结构、转变经济增长方式,改变扶贫开发观念和方式、完善基础设施建设、利用政策优势整合公共资源,加快实现县域经济的包容性增长,推进中部地区罗霄山片区扶贫攻坚进程。     

基于旅游非优区理论的森林公园旅游发展探讨——以陕西省翠峰山森林公园为例

基于旅游非优区理论,探讨了旅游非优区研究进展、优化路径,以陕西省翠峰山森林公园为例,分析了翠峰山的非优表现,总结出由"生态、创新、主题、本土、休闲、体验"六环节构成的公园旅游优化发展模式.森林公园非优区的旅游发展应突破传统的资源导向模式,结合市场需求与特点,以休闲经济和度假旅游为导向,合理定位、重新组合,开发休闲旅游资源,打造差异化的特色旅游产品;营造独树一帜的休闲度假环境;走出特色化的旅游管理与服务;塑造品牌化的旅游文化与形象,走不仅仅依靠资源的多向发展之路.     

长白山重点国有林区森林资源动态分析--以临江林业局为例

以临江林业局为例,分析了1977—2008年长白山重点国有林区森林资源动态变化情况,并提出今后森林资源经营管理的建议.结果表明:临江林业局林业用地面积和有林地面积均呈先下降后上升趋势,林地利用效率逐渐提高.1977—1997年,天然林面积逐年大幅减少,减少率约为37%,而后逐年上升;阔叶林蓄积所占比例大幅减少,针叶林蓄积比例大幅增加,针阔混交林蓄积占比趋向合理;1987年,中龄林面积和蓄积比例均很大;2008年林分各龄组面积和蓄积占比趋向合理.     

Sm-Nd isochron age of ophiolite along northern margin of Altun Tagh Mountain and its tectonic significance

An ophiolite belt is exposed to the northern edge of Altun Tagh Mountain. Geochronological researches were made on gabbro and basalt. Sm-Nd isochron age of gabbro is (829 ± 60) Ma, while the age of gabbro mixed basalt is (949 ± 62) Ma. The dating of Sm-Nd isochron proves that ophiolite formed in (829 ± 60) Ma, which implies that the northern half of Tarim (or north Tarim Block) had been separated by an ocean from the southern half of Tarim and Qaidarn (or south Tarim Block) until (829 ± 60) Ma. The south Tarim Block could accrete to the north Tarim Block at the beginning of Sinian, thereby forming the north Altun Tagh suture. The Sinian system would be the first cover on the amalgamated Tarim craton.     

The age of Xiannü Mountain fracture belt in Three-Gorge region——A fission track study

Apatite was separated from fault-clay, fracture-cliff rock and fracture wall rock, which were collected from Huangkou fracture north to Xiannu Mountain lying 20 km southwest to Three Gorges Dam Project-Sandouping dam. The fission tract characters and their length variations of apatite show that Xiannu Mountain fracture belt was formed at (0.7 ± 0.04)Ma, but its wall rock at (25.31 ±2.8) Ma. This result and previous studies show that no activity has happened since the Holocene, and the Three Gorges Dam Project is not affected by activity of the Xiannu Mountain fracture belt.