Analyses of Crustal Deformation,Strain Field and Risk of Moderate and Strong Earthquakes in the Shanxi Seismic Belt     

Wang Xiuwen  Zhao Xinping  Zhao Lihu  Peng Hao 《中国地震研究》2002,16(4):396-410

Using the four phases (1996～1999) of re-surveying data from the GPS network along the Shanxi fault zone, the recent state of horizontal movement of the fault zone and its relation with the Datong-Yanggao M5.6 earthquake (November 1, 1999), which took place on the north end of the monitored area, are analyzed. In the focal region, three areas with relatively higher strain (1×10 -6) appeared in Xinzhou and to the northeast of Jiexiu. The Shanxi fault zone is mainly controlled by the WNW-ESE-trending compressive stress field and the NNE-SSW-trending tensile stress field, and it does not have strike-slip movement. When examined for long-term tendency, attention should be paid to the junctures between the three moving elements.  相似文献   

广西西北部二叠系——三叠系界线碳、氧同位素组成异常及其意义   总被引：7，自引：0，他引：7       下载免费PDF全文

王大锐  王新平等 《地质论评》2001,47(3):225-228

我国广西西北部平果太平剖面二叠系－三叠系界线处为保存良好的海相碳酸盐岩沉积，根据牙形石化石带推断，该剖面在二叠系－三叠系界线处的连续沉积性良性。在该界线附近处，碳同位素组成发生了突然的负向波动，δ^13C从1．3‰－2．2‰（PDB）降至－0．9‰－－0．2‰，波动范围达2．8‰，进入下三叠统后一直呈负向发展；氧同位素组成波动虽不与碳同位素组成同步，但趋势相同，在二叠系－三叠系界线处达到最小值－8．2‰，下降幅度达2‰。这种同位素组成的波动已在我国西藏，浙江等的同时代的沉积中发现，此外，还在中东，北美洲，欧洲等地的二叠系－三叠系界线处发现，因此，它可以成为大区域及至洲际之间的二叠系－三叠系界线对比标志，这同时表明，二叠纪末期的重大地质事件发生的时间短，影响范围大，几乎是全球性的。  相似文献   

Simulations of Stable Isotopic Fractionation in Mixed Cloud in Middle Latitudes―Taking the Precipitation at ürǖmqi as an Example     

ZHANG Xinping  YAO Tandong  LIU Jingmiao  TIAN Lide  Masayoshi NAKAWO 《大气科学进展》2003,20(2):261-268

The introduced mathematical model takes into account the role of the kinetic fractionation effect in a supersaturation environment at the ice surface as liquid and solid phases coexist in mixed cloud. Using the model, the temperature effect of stable isotopes in precipitation is simulated under different cooling conditions. The rate of change of δ18O against temperature in the process of wet adiabatic cooling is smaller than in the process of isobaric cooling under the same humidity. The increasing supersaturation ratio at the ice surface, Si, leads to the strengthening of the kinetic fractionation effect. The kinetic fractionation function makes the synthesis fractionation factor decreased and the change of δ18O with temperature flatted, compared with that in the equilibrium state. The simulated results show that the slope parameter b and the intercept d of the meteoric water line (MWL), δD = bδ18O+d, in wet adiabatic cooling are both greater than those in isobaric cooling. The global MWL lies between the two MWLs simulated under wet adiabatic and isobaric cooling processes, respectively. The magnitudes of b and d are directly proportional to Si. The greater the Si, the stronger the kinetic fractionation effect, and thus the greater the b and d, and vice versa. However, b and d have low sensitivity to the liquid-water contents in the cloud. Using the kinetic fractionation model, the variation of stable isotopes in precipitation at Urumqi is simulated. The simulated stable isotopic ratio vs temperature and the δD vs δ18O curves are very consistent with the actual regressions and MWL at Uruimqi, respectively.  相似文献   

利用稳定同位素比率估计湖泊的蒸发   总被引：13，自引：2，他引：13  

章新平  姚檀栋 《冰川冻土》1997,19(2):161-166

利用稳定同位素物质平衡方法可以估算湖泊的蒸发，方法的主要特点是不必测定入湖水量，只须测定其稳定同位素比率。文章根据青海湖实测的氧同位素资料和有关水文气象资料，并利用稳定素模型得出，青海湖多年平均蒸发量为８７７ｍｍ，这个值与同一时期９０４．６ｍｍ的实测蒸发量大致相当，不同水体中稳定同位素比的大小对湖蒸发量有不同程度的影响。降水和入湖泊水中的稳定同位素比率与蒸发量存在正比关系；湖泊水和蒸发水中的稳定同  相似文献   

载体性质对Pt催化剂H₂选择催化还原NO_x活性和选择性的影响（英文）     

李新燕  张肖肖  徐永贞  柳叶  王新平 《甘肃地质》1997,(1):197-203

研究了Pt/MgO,Pt/γAl2O3Pt/ZrO2和Pt/HZSM-5催化剂上H选择催化还原消除NOxH2SCR)反应.结果发现,H2SCR活性和N2生成选择性受催化剂中Pt的金属性以及载体的氮氧化物吸附能力影响很大.HZSM-5的表面酸性使载体对NO吸附能力较小,使担载Pt以较高的金属性存在,从而导致Pt/HZSM-5催化剂的高活性和高选择性.相反,Pt/MgO和Pt/γAl2O3催化剂较差的活性和选择性可归因于其载体的碱性表面、催化剂中Pt较低的金属性以及载体对氮氧化物较大的吸附能力.结合反应的原位红外光谱结果可以认为,在Pt/载体界面处亚硝酸根/硝酸根物种被还原为N2或N2O取决于该处参与反应的活性H与这些含氮物种的相对数目.  相似文献   

运城盆地的现今构造活动及现代地壳应力场的基本特征   总被引：1，自引：0，他引：1  

刘巍  安卫平  赵新平 《山西地震》1996,(2)

大量震源机制解结果表明，运城盆地存在以水平拉张为主要特点的局部小区域应力场，盆地北部水平挤压分量占优势。这些特点不同于山西断陷带其它诸盆地局部小区域应力场的特点。由这些震源机制解结果中所有Ｐ轴、Τ轴做出的运城盆地的平均应力场，与华北区域地壳应力场和山西平均应力场的结果基本一致。说明运城盆地在宏观上、整体上仍严格受华北区域应力场的控制，其局部小区域应力场也是在华北区域应力场范畴内活动  相似文献   

基于人工神经网络的边坡稳定性工程地质评价方法   总被引：34，自引：0，他引：34  

夏元友  李新平 《岩土力学》1996,17(3):27-33

针对边坡稳定性工程地质评价方法过分强调经验和难以定量的缺点，提出了一种基于人工神经网络的边坡稳定性工程地质评价方法（ＡＮ２Ｓ２ＥＧＥＭ），详细介绍了它的建模方法和应用实例．结果表明该方法不仅有效，而且有定量、简便、实时、自适应等优点，具有广阔的应用前景。  相似文献   

Laser probe <Superscript>40</Superscript>Ar-<Superscript>39</Superscript>Ar ages of metasomatic K-feldspar from the Hougou gold deposit,northwestern Hebei Province,China     

Xingwang?Xu  Xinping?CaiEmail author  Yulin?Liu  Baolin?Zhang 《中国科学D辑(英文版)》2002,45(6):559-564

The Hougou gold deposit in northwestern Hebei is a typical K-metasomatism-related gold deposit hosted by K-altered rocks overprinting alkali intrusive rocks. In order to determine the age and pulse intervals of K-metasomatism in this gold deposit, some metasomatic K-feldspars from K-altered rocks are selected to measure their formation time by laser probe ⁴⁰Ar-³⁹Ar dating method. The new analyzing data show that these metasomatic K-feldspar formed during 202.6 Ma and 176.7 Ma, and the corresponding K-metasomatism and associated gold mineralization occurred in the early stage of Mesozoic era. The pulse intervals of K-metasomatism in the Hougou area are estimated to be about 4 Ma.  相似文献   

基于WebGIS的气象服务产品制作系统及关键技术   总被引：1，自引：1，他引：0       下载免费PDF全文

吕终亮  白新萍  薛峰 《应用气象学报》2018,29(1):120-128

基于WebGIS技术采用服务即是软件、软件即是服务的建设思路,结合可扩展框架技术,实现基于服务集成的气象服务产品在线制作系统的建设,从一定程度上解决了系统产品制作面临的不能集中部署、规范不统一、效率低下、更新复杂等问题。系统分为服务器端和客户端两部分,服务器端负责服务接口的开发和发布,客户端负责各级调度管理和运行。该系统解决了服务的注册、标准化、流水线化、参数序列化、多级任务调度等多个关键技术,系统具备可扩展性、产品标准化、流程规范化、跨平台等特点,系统建设的完成增加了气象服务产品制作的规范性、接口化,产品制作时间由原来的1~2 min降至10 s以内。  相似文献   

MATHEMATICAL MODELING OF VARIATIONS ON STABLE ISOTOPIC RATIOS IN FALLING RAINDROPS^*     

Zhang Xinping  Xie Zichu  Yao Tandong 《Acta Meteorologica Sinica》1998,12(2):213-220

The variations of stable isotopic contents in falling raindrops are not only influenced by the humidity conditions, but also by the stable isotopic contents in atmospheric vapor to a certain extent. If there is a difference between the isotopic contents in the vapor of the surrounding air and at the surface of the raindrops, the move of the isotopic contents from high to low values will be produced. Usually. influenced by the evaporation process, the stable isotopic ratios in raindrops are constantly increased in the unsaturated atmosphere. The less the atmospheric humidity, the more obvious the increased range. As the enrichment rate of stable isotopes in raindrops is equal to the outward isotopic move rate. the "pseudo-equilibrium state" appears. The influence of evaporation on stable isotopic contents disappears in the saturated atmosphere, so that the magnitude of isotopic ratio in raindrops is dependent on the isotopic exchange between the raindrops and the surrounding atmosphere.  相似文献