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褚绍唐先生是中国著名的地理教育家,历史地理学家,华东师范大学地理系教授。褚先生的地理教育思想构建起了中国中小学地理教育教学与研究的基本框架,先生组织发起的地理教育学术组织和创办的学术期刊仍发挥着巨大作用,先生编写的中小学地理教学大纲和教材惠及数代人。褚先生对上海历史地理的研究颇有建树,对上海的城市发展过程、成陆过程,水系变化等有独特见解。褚先生对《徐霞客游记》的整理和校点工作具有划时代意义,同时,先生也是徐霞客研究领域的大师。此外,褚先生还在城市地理学、地图学、地理文献翻译等领域做出了贡献。 相似文献
3.
Ailixiati Yushan Liu Daiqin Li Jie Li Rui Abudutayier Yasen Sun Xiaoxu Zhu Zhiguo Li Guirong Chen Li 《中国地震研究》2018,32(3):377-387
This paper analyzes the characteristics of time sequence changes of gravity points near the epicenter, different changes of measuring lines and gravity changes of measuring areas in point-line-area manner respectively with the 5-period mobile gravity data through densified observation by the South Xinjiang Observation Network after the 2015-2016 Akto earthquake in Xinjiang. The gravity observation results before the earthquake indicate that the Wuqia-Bulungkol area near the epicenter presented the trend of gravity value increasing since 2015, but the gravity value decreased half a year before the earthquake, and witnessed a high gradient zone of gravity changes during some periods before the earthquake. The gravity observation results after the earthquake show that there is a trend of opposite changes in gravity difference on the northern and southern sides of Bulunkou, and good correspondence exists between the characteristics of gravity field changes near the epicenter before and after the earthquake and the geologic structure distribution in the area. 相似文献
4.
陕西省山阳县香沟钨矿是近年来南秦岭地质勘查新发现的钨矿化地段之一。本文开展了白钨矿电子探针、LA-ICP-Ms和共生方解石的Sm-Nd同位素测年,研究结果显示：香沟白钨矿成矿过程至少可划分为两个阶段,由早阶段韵律环带白钨矿至晚阶段集合体状白钨矿,白钨矿经历了多次迁移;白钨矿具有高F、含微量Au元素的特征,稀土总量较高（ΣREE+Y含量介于5.44×10-6~382.67×10-6,平均为95.48×10-6）,其稀土配分型式为无MREE富集的平坦型,与Ghaderi等人划分的白钨矿Ⅱ型稀土配分型式总体类似,负铕异常,利用白钨矿La-Ce-Y三角图解,结合地质事实,判断香沟钨矿属于石英脉型钨矿;结合共生方解石Sm-Nd同位素年龄195 Ma,认为南秦岭香沟钨矿是印支末期深部隐伏岩浆-热液活动的结果。 相似文献
5.
本文在梳理流域地下水资源评价现状及历史的基础上,讨论了水资源评价方法和分区原则,将珠江流域划分为129个四级地下水系统,以地下水系统为评价单元,在充分考虑不同水文地质参数的基础上,分析评价地下水资源量及存在的问题,讨论珠江流域三级阶地不同水流运动特征,阐述了评价的精度以及水利工程对地下水循环的影响。通过本次评价,珠江流域地下水天然资源量1374.16亿m~3,可开采量为578.7亿m~3,开发利用率仅10.01%。珠江流域跨度较大,水动力特征迥异:上游云贵高原深切峡谷区、中游桂中峰丛洼地区、下游冲洪积平原区,据不完全统计,珠江流域蓄水量大于100万m~3的水库32座,水利工程的修建以及水库对水资源调蓄和分配给地下水资源评价带来一定困难,不同部委对地表水和地下水概念上的分歧导致二者间流域边界不一致以及流域水资源评价结果的差异,为此提出了解决问题的建议,以期为地下水开发利用与治理保护服务。 相似文献
6.
无人机倾斜摄影测量颠覆了以往正射影像只能从垂直角度拍摄的局限,在三维建模中有广泛的前景。针对有些无人机倾斜影像数据无相机标定参数、无航带信息（无序）、无POS信息的现状,本文以计算机视觉中基于内容的影像检索方法与改进的渐进式SFM方法为基础,提出一种“三无”影像自动检索、空中三角测量及影像三维重建的方法。该方法首先通过提取的特征检索出相似影像并建立网络结构,然后将影像进行两两匹配增强对应关系并进行连接点的追踪,最后利用光束法平差方法对其进行平差,获取影像集的三维点云,提高大规模影像检索、影像匹配速度的同时,提高重建的精确性和鲁棒度。本文选取三组典型试验区大数据量倾斜影像数据进行试验,立体实测控制点中误差可以达到平面0.16m/高程0.18m,试验验证了方法的稳定性、可靠性和实用性。 相似文献
7.
The three most crucial factors for the formation of large and super-large magmatic sulfide
deposits are: (1) a large volume of mantle-derived mafic-ultramafic magmas that participated in the
formation of the deposits; (2) fractional crystallization and crustal contamination, particularly the input
of sulfur from crustal rocks, resulting in sulfide immiscibility and segregation; and (3) the timing of
sulfide concentration in the intrusion. The super-large magmatic Ni-Cu sulfide deposits around the world
have been found in small mafic-ultramafic intrusions, except for the Sudbury deposit. Studies in the past
decade indicated that the intrusions hosting large and super-large magmatic sulfide deposits occur in
magma conduits, such as those in China, including Jinchuan (Gansu), Yangliuping (Sichuan), Kalatongke
(Xinjiang), and Hongqiling (Jilin). Magma conduits as open magma systems provide a perfect environment
for extensive concentration of immiscible sulfide melts, which have been found to occur along deep
regional faults. The origin of many mantle-derived magmas is closely associated with mantle plumes,
intracontinental rifts, or post-collisional extension. Although it has been confirmed that sulfide immiscibility
results from crustal contamination, grades of sulfide ores are also related to the nature of the
parental magmas, the ratio between silicate magma and immiscible sulfide melt, the reaction between
the sulfide melts and newly injected silicate magmas, and fractionation of the sulfide melt. The field relationships
of the ore-bearing intrusion and the sulfide ore body are controlled by the geological features of
the wall rocks. In this paper, we attempt to demonstrate the general characteristics, formation mechanism,tectonic settings, and indicators of magmatic sulfide deposits occurring in magmatic conduits which
would provide guidelines for further exploration. 相似文献
8.
By using the finite element method and viscoelastic artificial boundary,a soil-structure interaction system is established to simulate the influence of surface buildings on the seismic response of subway structures.The conditions of different relative positions between ground building and subway structure are analyzed.The results indicate that when considering the existence of surface buildings,the relative story displacements and internal forces of subway structures are changed greatly.Further the influence of surface buildings on subway structure changes as the distance increases. 相似文献
9.
Based on Fourier-Bessel series expansion of wave functions,an analytical solution to 2-D scattering ofincident plane SV waves by circular cylindrical canyons with variable depthto-width ratios is deduced in this paper. Unlike other analytical solutions,this paper uses the asymptotic behavior of the cylindrical function to directly define the undetermined coefficients of scattered waves,thus,avoiding solving linear equation systems and the related numerical computation problems under high-frequency incident waves,thereby broadening the applicable frequency range of analytical solutions. Through comparison with existing analytical solutions,the correctness of this solution is demonstrated. Finally, the incident plane SV wave scattering effect under circular cylindrical canyons in wider frequency bands is explored. 相似文献
10.