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661.
Suofei Xiong Mouchun He Shuzhen Yao Yubao Cui Guanzhong Shi Zhenju Ding Xinlu Hu 《Geological Journal》2015,50(6):720-738
The Chalukou giant Mo deposit in the Heilongjiang Province, northeastern China, is a porphyry deposit hosted in an intermediate‐felsic complex surrounded by Mesozoic volcano–sedimentary rocks. The mineralization process is composed of four stages, including quartz + K‐feldspar (Stage I), quartz + molybdenite (Stage II), pyrite + chalcopyrite + quartz ± other sulphides (Stage III) and carbonate ± fluorite ± quartz (Stage IV). The mineralization is generally associated with intense K‐feldspar‐, fluorite‐, phyllic‐ and propylitic alteration. Primary fluid inclusions (FIs) in quartz include four compositional types, i.e. pure carbonic (PC‐type), aqueous‐carbonic (C‐type), daughter mineral‐bearing (S‐type) and aqueous (W‐type) inclusions. Halite, sylvite and hematite are recognized as the daughter minerals in Stage I S‐type FIs, whereas molybdenite and chalcopyrite occur as daughter minerals in Stage II S‐type FIs. High‐salinity and high pressure (>220 MPa) FIs exist in Stage I quartz veins, characterized by homogenization through halite dissolution at temperatures of 324 to 517 °C. The paucity of coexisting vapour‐rich FIs with similar homogenization temperatures at this stage indicates that the initial S‐type inclusions have directly exsolved from the magma rather than boiling off of a low‐salinity vapour. Stage I quartz has captured the C‐ and W‐type FIs, which have totally homogenized at 270–530 °C with salinities of 1.6–17.0 wt.% NaCl equiv. At Stage II, the coexistence of all FI types were only observed at pressures of 150–218 MPa and temperatures of 352–375 °C, with two salinity clusters of 0.9–16.6 wt.% NaCl equiv. and 37–56 wt.% NaCl equiv. Stage III quartz contains W‐type FIs with homogenization temperatures of 158–365 °C, salinities of 0.5–9.0 wt.% NaCl equiv., and minimum pressures of 12–116 MPa; whilst Stage IV fluorite or calcite only contains W‐type FIs with homogenization temperatures of 121–287 °C, salinities of 0.5–5.3 wt.% NaCl equiv., and minimum pressures of 10–98 MPa. The estimated trapping pressure from Stages II to III suggests an alternating lithostatic–hydrostatic fluid‐system caused by fluid boiling. Ore fluids at the Chalukou Mo deposit may have been evolved from a CO2‐rich, high‐salinity, and high‐oxygen fugacity (fO2) magma system, to a CO2‐poor, low‐salinity, and low‐fO2 epithermal system. Two key points may have contributed to the formation of the Chalukou giant Mo deposit: The magmatic origin and fluid boiling that has resulted in decompression and rapid precipitation of metals. Copyright © 2014 John Wiley & Sons, Ltd. 相似文献
662.
Effects of grazing exclusion on plant productivity and soil carbon,nitrogen storage in alpine meadows in northern Tibet,China 总被引:4,自引:1,他引:3
Grazing exclusion is widely adopted in restoring degraded alpine grasslands on the Qinghai-Tibetan Plateau. However, its effectiveness remains poorly understood. In this study, we investigated the effects of grazing exclusion on plant productivity, species diversity and soil organic carbon (SOC) and soil total nitrogen (STN) storage along a transect spanning from east to west of alpine meadows in northern Tibet, China. After six years of grazing exclusion, plant cover, aboveground biomass (AGB), belowground biomass (BGB), SOC and STN were increased, but species diversity indices declined. The enhancement of AGB and SOC caused by grazing exclusion was correlated positively with mean annual precipitation (MAP). Grazing exclusion led to remarkable biomass increase of sedge species, especially Kobresia pygmaea, whereas decrease of biomass in forbs and no obvious change in grass, leguminous and noxious species. Root biomass was concentrated in the near surface layer (10 cm) after grazing exclusion. The effects of grazing exclusion on SOC storage were confined to shallow soil layer in sites with lower MAP. It is indicated that grazing exclusion is an effective measure to increase forage production and enhance soil carbon sequestration in the studied region. The effect is more efficient in sites with higher precipitation. However, the results revealed a tradeoff between vegetation restoration and ecological biodiversity. Therefore, carbon pools recover more quickly than plant biodiversity in the alpine meadows. We suggest that grazing exclusion should be combined with other measures to reconcile grassland restoration and biodiversitv conservation. 相似文献
663.
Tidal data from Weizhou, Zhapo, and Shanwei stations between 1969 and 2010 and from five gauging stations in the western Pacific Ocean provided by PSMSL, and the global mean sea level data recorded between December 1992 and December 2010 by TOPEX and Jason satellites were compiled and analyzed. The results show that the perennial mean sea level near Weizhou Island is 211.7 cm(relative to the water gauge zero), and the relative mean sea level rising rate is 2.2 mm yr-1 from 1969 to 2010, which is consistent with the relative mean sea level rising rate recorded at other gauging stations in the western Pacific regions and with the global mean sea level rising rate. The absolute mean sea level rising rate at Weizhou Island is 3.0 mm yr-1 from 1993 to 2010, also conforming with the global mean sea level rising rate(3.1±0.4 mm yr-1) during the same time period. The highest annual tide level at Weizhou Island has a rising rate of 4.6 mm yr-1 and shows a 20-year quasi-periodic variation from 1966 to 2010. The primary cause of the mean sea level rising is global warming. 相似文献
664.
Standards of ecological compensation for traditional eco-agriculture: Taking rice-fish system in Hani terrace as an example 总被引:10,自引:2,他引:8
Mou-cheng Liu Yin Xiong Zheng Yuan Qing-wen Min Ye-hong Sun Anthony M. Fuller 《山地科学学报》2014,11(4):1049-1059
Traditional eco-agriculture provides many ecosystem services which are important for the local environment, especially in mountain areas. In order to encourage the farmers to engage in eco-agriculture,it is necessary to establish an eco-compensation mechanism for them. As the compensation standard is one of key issues in establishing eco-compensation mechanism, this paper calculated the standard based on the farmers' willingness to accept(WTA) and the input-output analysis of eco-compensation. We took the traditional rice-fish eco-agriculture as the research object, conducting field surveys in Hani Terrace of Honghe County. Through the questionnaires in 2011, we obtained the farmers' willingness to accept government compensation and market compensation. Then, the research evaluated the output of eco-compensation, the economic value of rice-fish paddy ecosystem services. Finally, under different market compensation standards, we compared the input and output of government compensation. The results show that, in 2011 the government should to pay farmers 7462 yuan·ha–1·a-1to meet their willingness, but the output(ecological benefit) was only 7393 yuan·ha–1·a-1. However, when the rice price increases 1 yuan·kg-1 because of the limited use of chemicals in the next year, the government just has to pay farmers 4062 yuan·ha–1·a-1 and the surplus will be 3331 yuan·ha–1·a-1. 相似文献
665.
兵棋是对作战过程进行逻辑推演研究和评估的军事科学工具,其三大组成要素包括棋盘、棋子和规则。棋盘的经典样式就是六角格兵棋棋盘,计算机兵棋中也常采用六角格棋盘描述战场地形环境,而棋盘的投影变形和坐标转换分别是制约兵棋推演可信度和推演效率的重要因素。首先分析了棋盘所用投影方式的变形规律,提出了个体值法和平均值法对变形进行修正;然后针对经纬度坐标和六角格编码的转换,提出了直接转换和间接转换两种方法,分析其基本转换原理,并给出了坐标转换公式;最后通过实验对所述方法进行验证,结果证实平均值法对于修正投影变形具有很好的实用性,且间接坐标转换法具有更高的转换效率。 相似文献
666.
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668.
计算机技术引入地图学之后,引起地图制作与生产方式的极大变革.地图设计作为地图制作的核心,其内涵也发生了重要变化.以电子地图的多尺度表达为目标,探讨了地图设计在时空尺度上的扩展,提出了多尺度地图设计模型.为地图设计知识的抽象化、可视化以及设计知识向普通大众的传播提供了可借鉴的样本. 相似文献
669.
Analogue-dynamical prediction of monsoon precipitation in Northeast China based on dynamic and optimal configuration of multiple predictors 下载免费PDF全文
Based on the National Climate Center (NCC) of China operational seasonal prediction model results for the period 1983–2009
and the US National Weather Service Climate Prediction Center merged analysis of precipitation in the same period, together
with the 74 circulation indices of NCC Climate System Diagnostic Division and 40 climate indices of NOAA of US during 1951–2009,
an analogue-dynamical technique for objective and quantitative prediction of monsoon precipitation in Northeast China is proposed
and implemented. Useful information is extracted from the historical data to estimate the model forecast errors. Dominant
predictors and the predictors that exhibit evolving analogues are identified through cross validating the anomaly correlation
coefficients (ACC) among single predictors, meanwhile with reference of the results from the dynamic analogue bias correction
using four analogue samples. Next, an optimal configuration of multiple predictors is set up and compared with historical
optimal multi-predictor configurations and then dynamically adjusted. Finally, the model errors are evaluated and utilized
to correct the NCC operational seasonal prediction model results, and the forecast of monsoon precipitation is obtained at
last. The independent sample validation shows that this technique has effectively improved the monsoon precipitation prediction
skill during 2005–2009. This study demonstrates that the analogue-dynamical approach is feasible in operational prediction
of monsoon precipitation. 相似文献
670.