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91.
新疆阿尔泰克因布拉克铜锌矿床地质特征及成矿作用   总被引:4,自引:1,他引:3  
克因布拉克中型铜锌矿床赋存于早二叠世花岗岩外接触带的上志留统-下泥盆统康布铁堡组黑云石英片岩、变质石英砂岩中。矿床的形成经历了夕卡岩期、热液期和表生期,铜锌矿主要形成于热液期。矿石中石英和方解石流体包裹体划分为H_2O-NaCl型和H_2O-CO_2(±CH_4/N_2)-NaCl型。成矿温度变化于146~448℃,在170℃、270℃和350℃出现峰值;流体盐度变化于0.2%~46.9%NaCl_(eq),峰值为1.5%NaCl_(eq)和5.5%NaCl_(eq);流体的密度0.55~1.19g/cm~3。硫化物的δ~(34)S集中变化于-8.4‰~1.9‰,峰值为0‰,表明硫来自岩浆。石英和方解石δD_(SMOW)介于-130‰~-79‰,δ~(18)O_(SMOW)值介于8.0‰~11.6‰,δ~(18)O_(H2O)值为-1.7‰~4.43‰,表明成矿流体主要是岩浆水,混合大气降水。方解石中δ~(13)C_(PDB)变化于-5.3‰~-1.1‰,暗示碳来自花岗质岩浆。成矿时代为早中二叠世,成矿作用与花岗质岩浆期后的热液活动有关。  相似文献   
92.
本文基于对地质学的深刻认识、对传统文化的热爱及对社会现象的观察,系统而深刻地提出了"地质文化"的概念,首次描述了地质文化的基本框架、建设原则及实例片段。地质文化建设将对地质学及我国的文化建设有着实质性的推动作用,是构建和谐社会的重要组成部分。  相似文献   
93.
The spatial and temporal variation of major ions (Ca2+, Mg2+, Na+, K+, , , and Cl) in Himalayan snow and ice is investigated by using two snow pits from the East Rongbuk glacier (28°01′N, 86°58′E, 6500 m a.s.l.), one snow pit from the Nangpai Gosum glacier (28°03′N, 86°39′E, 5700 m a.s.l.), one snow pit from the Gyabrag glacier (28°11′N, 86°38′E, 6303 m a.s.l.), and three ice cores from the Sentik (35°59′N, 75°58′E, 4908 m a.s.l.), Dasuopu (28°33′N, 85°44′E, 7000 m a.s.l.), and East Rongbuk (27°59′N, 86°55′E, 6450 m a.s.l.) glaciers, respectively. In general, the major ions show a significant seasonal variation, with high concentrations during the non-monsoon (pre-monsoon and post-monsoon) season and relatively low concentrations during the monsoon season. Monsoon precipitation with high local/regional dust loading related to summer circulation is possibly responsible for the high concentrations occurring sporadically during the monsoon season. The crest of the Himalayas is an effective barrier to the spatial distribution of Na+, Cl and concentrations, but not to the major ions associated with dust influx (e.g. Ca2+ and Mg2+). Atmospheric backward trajectories from the HYSPLIT_4 model used in identifying chemical species sourcing suggest that the major ions in the Himalayan snow and ice come mainly from the Thar Desert located in the North India, as well as West Asia, or even the distant Sahara Desert in the North Africa during the winter and spring seasons. This is different from the conventionally assumed arid and semi-arid regions of the central Asia. Factors, such as different vapor sources due to atmospheric circulation patterns and geographical features (e.g. altitude, topography), may contribute to the differences in major ionic concentrations between the western and eastern Himalayas.  相似文献   
94.
Tidal flats, a precious resource that provides ecological services and land space for coastal zones, are facing threats from human activities and climate change. In this study, a robust decision tree for tidal flat extraction was developed to analyse spatiotemporal variations in the Bohai Rim region during 1984-2019 based on 9539 Landsat TM/OLI surface reflection images and the Google Earth Engine (GEE) cloud platform. The area of tidal flats significantly fluctuated downwards from 3551.22 to 1712.36 km2 in the Bohai Rim region during 1984-2019, and 51.31% of tidal flats were distributed near the Yellow River Delta and Liaohe River Delta during 2017-2019. There occurred a drastic spatial transition of tidal flats with coastline migration towards the ocean. Low-stability tidal flats were mainly distributed in reclamation regions, deltas, and bays near the estuary during 1984-2019. The main factors of tidal flat evolution in the Bohai Rim region included the direct impact of land cover changes in reclamation regions, the continuous impact of a weakening sediment supply, and the potential impact of a deteriorating sediment storage capability. The extraction process and maps herein could provide a reference for the sustainable development and conservation of coastal resources.  相似文献   
95.
对基于能量平衡方程的多向随机波浪传播数学模型进行改进,通过模拟不同防波堤绕射引起的港池泊稳,验证模型的合理性和有效性。利用非线性弥散关系提高模型计算浅水变形的精度;采用二次逆风差分格式离散控制方程,避免了加入绕射项引起的数值耗散;并将文氏谱加入模型中,使其更加适合中国海域的工程应用。应用改进后模型绘制的双突堤和岛式防波堤绕射系数图与我国《海港水文规范》图进行了对比。对比结果十分接近,可以较好地描述港池的泊稳状况,为综合计算波浪在近岸的浅水变形、折射、绕射、反射和能量耗散等作用奠定了基础。  相似文献   
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98.
An overview of Chinese contribution to Coupled Model Intercomparison Project-Phase 5 (CMIP5) is presented. The performances of five Chinese Climate/Earth System Models that participated in the CMIP5 pro ject are assessed in the context of climate mean states, seasonal cycle, intraseasonal oscillation, interan-nual variability, interdecadal variability, global monsoon, Asian-Australian monsoon, 20th-century historical climate simulation, climate change pro jection, and climate sensitivity. Both the strengths and weaknesses of the models are evaluated. The models generally show reasonable performances in simulating sea surface tem-perature (SST) mean state, seasonal cycle, spatial patterns of Madden-Julian oscillation (MJO) amplitude and tropical cyclone Genesis Potential Index (GPI), global monsoon precipitation pattern, El Ni-no-Southern Oscillation (ENSO), and Pacific Decadal Oscillation (PDO) related SST anomalies. However, the perfor-mances of the models in simulating the time periods, amplitude, and phase locking of ENSO, PDO time periods, GPI magnitude, MJO propagation, magnitude of SST seasonal cycle, northwestern Pacific mon-soon and North American monsoon domains, as well as the skill of large-scale Asian monsoon precipitation need to be improved. The model performances in simulating the time evolution and spatial pattern of the 20th-century global warming and the future change under representative concentration pathways pro jection are compared to the multimodel ensemble of CMIP5 models. The model discrepancies in terms of climate sensitivity are also discussed.  相似文献   
99.
Vertical tilt structure of the East Asian trough (EAT) and its interannual variation mechanism in boreal winter are studied using NCEP/NCAR, ERA40, and NCEP/DOE reanalyses. A vertical tilt index (VTI) is defined as the mean slope of vertical trough line on the longitude-height cross section to describe the tilting extent of the EAT, with high index indicating a more west-tilted trough and vice versa. The VTI series derived from the three reanalysis datasets are highly correlated with each other during the corresponding periods. A significant positive correlation is found between the VTI and the zonal range of the vertical trough line. Based on the close relation, a possible physical mechanism is proposed to explain the interannual variation of VTI. It demonstrates that positive (negative) temperature anomalies within the mean zonal range of the EAT result in expansion (contraction) of the zonal range and lead to high (low) VTI years. The composite analyses based on the three reanalysis datasets well support the proposed mechanism. Furthermore, the general relationship between the VTI and the zonal temperature gradient is discussed based on the proposed mechanism. It is revealed that the asymmetric change of temperature gradient on the western and eastern sides of the EAT plays an important role in the variation of VTI, which suggests that the tilting extent of the EAT is strongly affected by the two-order zonal change of temperature instead of the zonal temperature gradient (i.e., one-order change). Climate variability not only in the simultaneous winter but also in the following spring and summer over East Asia is closely related to the variation of the VTI. This study on the vertical tilting of the EAT may enrich knowledge of the East Asian winter monsoon and the climate variability over East Asia and may be helpful in improving the regional climate prediction in East Asia.  相似文献   
100.
以南京市为例,构建人工蜂群元胞自动机(CAABC)模型,对2000—2007年的土地利用变化进行模拟以实现CAABC模型的校正,并以2007—2015年的土地利用变化为案例,验证该模型的有效性。模拟结果总体精度(OA)2007年为87.79%,2015年为80.61%;模拟结果的品质因数(FOM)2007年为21.23%,2015年为19.25%。基于CAABC模型和马尔可夫链预测未来城市土地总量,对南京市2025和2035年的土地利用格局进行了预测,对城市扩张和生态用地被侵占现象进行分析。模型预测结果表明,未来20年的城市扩张主要以牺牲耕地和林地为代价,2025和2035年80%的城市扩张面积来源于对耕地面积的侵占,17%的城市面积扩张是由2015年的林地转换得到的。研究表明,准确模拟、预测未来城市格局及评估城市扩张能够对生态用地侵占,以及为决策者合理规划城市、推动城市可持续发展提供帮助。  相似文献   
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