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671.
Liu Jiyuan Liu Mingliang Deng Xiangzheng Zhuang Dafang Zhang Zengxiang Luo Di 《地理学报(英文版)》2002,12(3):275-282
In the mid-1990s, we established the national operative dynamic information serving systems on natural resources and environment.
During building the land-use/land-cover change (LUCC) database for the mid-1990s, 520 scenes of remotely sensed images of
Landsat Thematic Mapper (TM) were interpreted into land-use/land-cover categories at scale of 1:100,000 under overall digital
software environment after being geo-referenced and ortho-rectified. The vector map of land-use/land-cover in China at the
scale of 1:100,000 was recently converted into a 1-km raster database that captures all of the high-resolution land-use information
by calculating area percentage for each kind of land use category within every cell. Being designed as an operative dynamic
information serving system, monitoring the change in land-use/land-cover at national level was executed. We have completed
the updating of LUCC database by comparing the TM data in the mid-1990s with new data sources received during 1999–2000 and
1989–1990. The LUCC database has supported greatly the national LUCC research program in China and some relative studies are
incompletely reviewed in this paper. 相似文献
672.
A two-dimensional,semi-geostrophic numerical model incorporating the tropopause andstratosphere is used to investigate the effects of a positive potential vorticity anomaly and latentheat release on the frontogenetic process and the structure of the resulting frontal zone.It isdemonstrated that(1)the inclusion of tropopause and stratosphere significantly changes the frontalstructure only in the upper levels;(2)a clearly defined quasi-equivalent barotropic structure and aregion of upward motion of finite width appear when a positive potential vorticity anomaly exists onthe warm side of the maximum baroclinity in the lower troposphere,especially when it is locatedon the south edge of the baroclinic zone;(3)the above mentioned structure deteriorates as thefrontogenesis proceeds in a dry atmosphere but can be maintained in a moist frontogenetic processwith condensational heating;(4)the combination of a positive potential vorticity anomaly and thelatent heat release is able to accelerate the frontogenesis significantly with the time needed to forman intense frontal zone reduced to less than 15 h.The results have significant theoreticalimportance in understanding the complex nature of frontal structure and frontogenesis,especiallyin understanding the dynamic structure of the subtropical frontal zone observed during earlysummer over East Asia. 相似文献
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676.
陕西省及汾渭地震带的发震概率 总被引:1,自引:1,他引:1
本文用韦布尔(Weibull)分布对陕西省及汾渭地震带的中强地震活动进行概率统计分析,得到所研究地区的中强地震平均复发周期和发震概率。通过陕西省及汾渭地震带的韦布尔概率模型可以获得任一预测时间内的发震概率。 相似文献
677.
Experimental data on windbreak flows have been analysed, using several statistical methods. Our analysis demonstrates that coherent structures exist in the mixing region of a porous windbreak (50% porosity) flow, and are largely responsible for the momentum transport that re-accelerates the leeward flow. A comparison between windbreak flow and laboratory turbulent mixing layers suggests that the dominant structures in these two flows are similar. Some previous numerical and experimental results are interpreted in light of the coherent structures and the self-similar property in the mixing region of a windbreak flow. 相似文献
678.
北京地区气温和降水百年变化规律的探讨 总被引:24,自引:0,他引:24
本文通过对北京地区120年气温和150年降水资料的分析发现:(1)年和季的平均气温变化有着明显的一致性,1920年是个转折点,前期偏低,后期偏高。(2)冬、夏季的极端最高气温近20年来呈偏低趋势,而极端最低气温呈持续偏高趋势。(3)年、季极端气温差值距平1972年以前以正距平为主,1972年以后以负距平为主。50年来差值持续变小。(4)北京与中国东部、北半球、全球平均气温在1920年以前趋势相同。1920年以后,北京和中国东部的趋势相同,而和北半球、全球有着明显的差别。(5)北京的年降水从50年代至80年 相似文献
679.
Petrogenesis of the granite related to the Baishaziling Sn deposit,Dayishan ore field,Southern China
Zhuang Zhao Xiaoyong Yang Wanying Li Tuyan Zhang Youyue Lu Zunzun Zhang 《Chemie der Erde / Geochemistry》2022,82(2):125873
The Baishaziling greisen-type tin deposit is located in the Dayishan ore field, Nanling Range, Southern China. In this study, for the first time, we present both zircon and cassiterite UPb dating, whole-rock elements, zircon LuHf and apatite Nd isotopic compositions to better constrain the petrogenesis of granite and its genetic link with Sn mineralization. Zircon UPb ages of fine-grained granite and coarse-grained granite are 154 ± 1.8 Ma and 153 ± 2.1 Ma, respectively, which are consistent with the cassiterite UPb dating of 154 ± 5.4 Ma, implying genetic relationship between the Baishaziling granite and tin metallogenesis. The Baishaziling granites exhibit high SiO2, K2O + Na2O, Zr + Nb + Ce + Y contents, low P2O5 and Sr contents, and high ratios of Ga/Al, TFeO/(TFeO + MgO), implying A-type granite affinity with characteristics of high-K calc-alkaline and weakly peraluminous. The zircon εHf(t) values and apatite εNd(t) values of the granite vary from ?4.46 to ?1.81 and ?8.37 to ?7.10, with two-stage Hf and Nd model ages of 1.40 to 1.50 Ga and 1.52 to 1.64 Ga, indicating that they were generated by the partial melt of the Proterozoic basement with the involvement of mantle magma. In addition, formation of Dayishan granite was likely associated with an intraplate extensional setting caused by the subduction of the Palaeo-Pacific plate. The Baishaziling reduced granites have high stannum and boron contents, which are in favor of the tin mineralization. 相似文献
680.
宁镇,茅山山脉褶皱逆冲一推覆构造带的构造岩类型主要为碎裂岩系列,其次为糜棱岩系列。主要超微构造为位错构造。经计算,区内印支、燕山期古差应力值约为90~100MPa,应变速率为:3.1x10~(-14)≤(?)≤2.0x10~(-10)。构造变形环境为低温、高压、高应变速率环境,微观机制主要为位错滑移。 相似文献