排序方式： 共有12条查询结果，搜索用时 15 毫秒
1.
High‐T and low‐P metamorphism in the Xilingol Complex of central Inner Mongolia,China: An indicator of extension in a previous orogeny 
下载免费PDF全文
下载免费PDF全文 The Xilingol Complex comprises biotite gneisses and amphibolite interlayers with extensive migmatization. Four representative samples were documented and found to record either two or three metamorphic stages. Phase modelling using thermocalc suggests that the observed assemblages represent the final stages that underwent cooling from temperature peaks, and are consistent with a fluid‐absent solidus in P–T pseudosections. Their P–T conditions are further constrained to be 5–6 kbar/680–725°C and 4–5 kbar/650–680°C for two garnet‐bearing gneiss samples, 4–5 kbar/660–730°C for a cordierite‐bearing gneiss sample, and 4–5 kbar/680–710°C for an amphibolite sample based on mineral composition isopleths, involving measured Mg content in biotite, anorthite in plagioclase, grossular and pyrope in garnet and Ti content in amphibole. The peak temperature conditions recovered are 760–790°C or >760°C at 5–6 kbar based on the composition isopleths of plagioclase, biotite, garnet and especially the comparison of melt contents between the calculated and observed. A pre‐peak heating process with slight decompression can be suggested for some samples on the basis of the core–rim increase in the plagioclase anorthite, and the stability of ilmenite. Zircon U–Pb dating using the LA‐ICP‐MS method provides systemic constraints on the metamorphic ages of the Xilingol Complex to be 348–305 Ma, interpreted to represent the post‐peak cooling stages. Moreover, metagabbroic dykes that intruded into the Xilingol Complex yield 317 ± 3 Ma from magmatic zircon, and are considered to have played a significant role for heat advection triggering the high‐T and low‐P metamorphism. Thus, the clockwise P–T paths involving pre‐peak heating, peak and post‐peak cooling recovered for the Xilingol Complex are consistent with an extensional setting in the Carboniferous that developed on a previous orogen in response to addition of mantle‐derived materials probably together with upwelling of the asthenospheric mantle. 相似文献
2.
选取内蒙古锡林郭勒盟与积雪有关的雪灾致灾指标， 以气温、 风速为气象条件孕灾环境指标， 坡度、 植被盖度为下垫面孕灾环境指标， 人口密度、 牧民纯收入、 人均GDP、 牲畜超载率等数据为承灾体脆弱性指标， 基于BP方法、 层次分析法、 建立了内蒙古锡林郭勒盟白灾综合风险评价体系， 并对其进行了风险评价与区划。为提高灾害评估的准确率， 白灾的灾害等级是以月为尺度进行评定， 选取的气象指标多数都是以月为尺度的指标。研究表明： 白灾与积雪因子高度相关， 是气候灾害， 积雪、 低温、 大风等气象因子长期作用的结果。对白灾尝试用BP神经网络法进行风险评估， 评估的灾害等级和实际灾害等级十分吻合， 用训练好的神经网络对各个旗县（1980 - 2015年）的白灾进行了风险评估， 评估效果理想。因此， 可以通过数值预报产品、 气候预测产品获取相关评价因子， 采用BP方法形成白灾风险预评估产品， 进而应用于雪灾风险评估业务中， 为相关部门提供决策依据。 相似文献
3.
生态系统服务功能动态区划方法与应用 总被引：2，自引：0，他引：2
开展区域生态系统服务功能动态区划,对生态系统服务功能的分区管理具有重要的指导价值。本文介绍了生态系统服务功能区划的方法--生态系统服务功能动态区划系统(SIZES)。该方法包括生态系统服务功能多层次表征、位序矩阵生成、核心生态系统服务功能空间辨识和动态区划边界生成四个模块,它们能实现生态系统服务功能动态区划边界的生成。其中,生态系统服务功能多层次表征模块和动态区划边界生成模块是主要模块,而构建生态系统服务功能表征指标体系和生成区划单元是该方法的关键所在。利用SIZES将锡林郭勒盟划分为6个生态系统服务功能区,科学合理地解释了该区生态系统服务功能空间分异规律,为指导该区生态系统服务功能分区管理,提供了具有时空特性的决策参考信息。 相似文献
4.
锡林郭勒牧区聚落体系演化特征及其机制 总被引：3，自引：3，他引：0
以锡林郭勒牧区（9旗市）145个规模以上聚落为研究客体,采用全国5次（1964年、1982年、1990年、2000年、2010年）人口普查数据及2015年调查数据,运用GIS空间分析技术、空间统计技术等方法,对研究区聚落体系的结构形态、规模等级、时空演变特征及机制进行分析。结构形态的动态特征表明,一定程度的外在作用力对地理环境基底均衡性产生影响,进而将对Christaller景观产生重大影响;规模等级的动态特征在不同时期遵循严格的规模-位序法则;50 a间,聚落规模总体变化速率基本与历史上的“大事件”一一对应。锡林郭勒牧区聚落体系的演化特征及其机制表明,经典的中心地体系在典型牧区依然受传统因素的影响,而当前对中心地体系影响深刻的信息化、网络化等因素在牧区未产生显著影响。另外,促使聚落体系演变的驱动因素以外因为主,内生动力不足为其主要特征。总体认为,锡林郭勒牧区聚落体系的时空演化特征对蒙古高原人地关系系统的调控与优化具有重要参考价值。 相似文献
5.
本文基于综合指数法构建生态脆弱性模型,借助质心迁移、趋势分析对锡林郭勒近20年生态脆弱性的时空演变进行了分析,并探究了自然因素和社会因素对生态脆弱性的驱动影响及时空分异特征。结果表明:①时间上,锡林郭勒生态脆弱性整体有所改善、分区特征显著。矿区、牧区生态治理成效显著;农业区生态脆弱性出现退化,需加强治理。②空间上,锡林郭勒生态脆弱性呈阶梯式分布,生态脆弱性质心逐渐向东偏移。西部地区生态脆弱性持续改善;中、东部地区生态脆弱性相对平稳,局部地区出现退化。③自然因素对空间尺度下的生态脆弱性主导特征显著,社会因素对时间尺度下的生态脆弱性主导特征逐渐增强。 相似文献
6.
基于RWEQ的20世纪90年代以来内蒙古锡林郭勒盟土壤风蚀研究 总被引：8，自引：1，他引：7
土壤风蚀是中国北方地区重要的生态环境问题。锡林郭勒盟位于中国干旱、半干旱地区,是中国北方典型风蚀区,其特殊的地理位置又使得本区成为华北重要的生态屏障,为此锡林郭勒盟全区均划入了京津风沙源治理工程区。为了更好地阐明锡林郭勒盟的土壤风力侵蚀过程,指导区域的荒漠化防治,,基于气象、遥感数据,利用RWEQ模型定量分析了20 世纪90 年代以来锡林郭勒盟的土壤风蚀时空格局,揭示土壤风蚀的主要影响因素。研究表明：锡林郭勒盟多年平均土壤风蚀量为3.39 亿t。土壤风蚀强度以微度和轻度为主,主要集中在植被较好,风蚀力较低,降雨量较高,雪被覆盖地表时间较长的东、中部地区以及南部地区。侵蚀强度为中度以上的侵蚀区集中在苏尼特右旗、正镶白旗和正蓝旗的浑善达克沙地;90 年代以来,锡林郭勒盟的土壤风蚀强度总体上呈减弱趋势,主要与风场强度的减弱,植被盖度等的变化有关。土壤风蚀多发生于风蚀力较大的春季,风蚀强度较大区域的春季植被盖度与风蚀量呈显著负相关（r>0.7,p<0.01）,且近20 年植被盖度提升有效降低了该区域的土壤风蚀。 相似文献
7.
Quantitative estimations of the fractional cover of photosynthetic vegetation (fPV), non-photosynthetic vegetation (fNPV) and bare soil (fBS) are critical for soil wind erosion, desertification, grassland grazing, grassland fire, and grassland carbon storage studies. At present, regional and large-scale fPV, fNPV and fBS estimations have been carried out in many areas. However, few studies have used moderate resolution imaging spectroradiometer (MODIS) data to perform large-scale, long-term fPV, fNPV and fBS estimations in the Xilingol grassland of China. The objective of this study was to quantitatively estimate the time series of fPV, fNPV and fBS in the typical grassland region of Xilingol from MODIS image data. Field measurement spectral and coverage data from May and September 2017 were combined with the 8-day composite product (MOD09A1) acquired during 2017. We established an empirical linear model of different non-photosynthetic vegetation indices (NPVIs) and fNPV based on the sample scale. The linear correlation between the dead fuel index (DFI) and fNPV was best (R2 = 0.60, RMSE = 0.15). A normalized difference vegetation index (NDVI)-DFI model based on MODIS data was proposed to accurately estimate the fPV, fNPV and fBS (estimation accuracies of 44%, 71%, and 74%, respectively) in the typical grasslands of Xilingol in China. The fPV, fNPV and fBS values for the typical grassland time series estimated by the NDVI-DFI model were consistent with the phenological characteristics of the grassland vegetation. The results show that the application of the NDVI-DFI model to the Xilingol grassland is reasonable and appropriate, and it is of great significance to the monitoring of soil wind erosion and fires in grasslands. 相似文献
8.
基于MSS、TM、ETM+以及HJ-1等遥感影像,构建内蒙古锡林郭勒盟1975~2009年长时间序列生态系统宏观结数据库,分析区域生态系统空间分布格局、动态变化及驱动机制。研究表明:①草地生态系统是锡林郭勒盟主体生态系统,草地占全区总面积比例始终在86%以上。②锡林郭勒盟生态系统演变过程明显以2000年为界:2000年前草地生态系统持续、加速萎缩,荒漠、农田等生态系统不断扩张;2000年后草地生态系统萎缩迅速得到遏制和逆转,农田和荒漠等生态系统扩张趋势也得到遏制。③区域气候变化及人类土地利用活动对生态系统演变有显著加速和减速作用。 相似文献
9.
Zoning grassland protection area using remote sensing and cellular automata modeling—A case study in Xilingol steppe grassland in northern China 总被引：1，自引：0，他引：1
Grassland degradation has become a serious environmental problem in China due to climate variability and human disturbances in the arid and semi-arid areas. Establishing grassland protection areas (GPAs) is regarded as an effective measure to protect grassland. This paper presents a new method to support the local government's effort in zoning of GPAs. It integrates a cellular automata (CA) model with geographical information system (GIS) and remote sensing. The proposed method includes two major steps: 1. to extract “seed points” of candidate GPAs using remote sensing techniques and GIS; 2. to simulate the zoning of GPAs using a CA model. The performance of the proposed method is evaluated using a case study in Xilingol steppe grassland in Inner Mongolia Autonomous Region of China. The results show that the integrated approach can rapidly find candidate GPAs that satisfy the zoning requirement. It has demonstrated that the proposed method of grassland protection zoning provides valuable decision support tools for government and planning agencies. 相似文献
10.
对植被的动态监测可以从一定程度上反映气候变化趋势。该文利用2000—2005年MODIS NDVI数据对锡林郭勒盟典型草原植被变化进行动态监测,在此基础上,以降水量、水汽压、平均气温、最高气温、最低气温、日照时数作为气候指标,分析锡林郭勒盟典型草原和荒漠草原MODIS NDVI与同期及前期气候因子的相关性,探讨草原植被变化的气候驱动因子。结果表明:2000—2005年锡林郭勒盟植被改善面积大于退化面积,植被退化面积最大的区域为荒漠草原,占全盟面积的12.84%,植被改善面积最大的区域为典型草原,占全盟面积29.09%。4类草原改善趋势由强到弱的顺序为草甸草原、典型草原、沙地草原、荒漠草原。对于典型草原,其NDVI与最高气温关系最密切,其次为水汽压;对于荒漠草原,其NDVI与最高气温关系最为密切,其次为最低气温。此外,NDVI对气候因子的响应表现出明显的时滞效应。 相似文献