GEOCHEMICAL EFFECTS OF MAJOR ELEMENTS DURING FLUID-ROCKS INTERACTION IN MARINWOBO FAULT IN THE SOUTH MARGIN AREAS OF ALTAI MOUNTAINS

There are four types of metamorphic rocks in the Marinwobo fault, i. e, cataclasite, mylonite,mictosite and migmatitic granite, and the formation of these rocks is due to the progressive metamorphism of the pyroclastics. The fluids play a very important role in the metamorphic process of these rocks in the Marinwobo fault, the most important feature is that the fluids not only result in the migration of the major elements of the deformation rocks, but also result in the volume loss of the deformation rocks in the deformation process. Thus the migration laws of the major elements in different stages of the progressive metamorphic process are discussed according to mass balance equations. Finally, the quantitative analysis of the mass loss and volume loss of the different rocks the in Marinwobo fault is discussed in this paper.     

SOME EXAMPLES OF TRANSITION SPANS MINERALIZING AND ANALYSIS OF THEIR DYNAMICS

The transitional span is a special environment for deposits. Taking peat, oil-gas, metallic deposits as examples, this paper discusses the spatial-temporal transitional characteristics of mineralization in transitional regions, points out the importance of the mineralization in transition spans, and analyses their dynamics finally.     

The medium- and short-term prediction methods of strong earthquakes based on neural network

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河流-含水层系统数值模拟方法探讨

地表水与地下水转化量的模拟预测一直是区域水资源评价和管理中的难题。提出了一种基于河流越流系数的处理方法,即将转化量计算模型同三维地下水数值模型完全耦合,能够预测在有人工干预条件下,地表水与地下水转化量的变化趋势。提出的方法适合多含水层系统的情形。实例研究表明,提出的河流-含水层系统模拟方法原理简单,易于实现,可以推广应用。     

Geodatabase数据模型驱动的人防地理数据库

为有效地组织人防资源和信息,为人防战时指挥和日常演习提供保障,提出了面向Geodatabase数据模型的人防地理信息系统数据库。该数据库依据地理空间数据标准来确定空间数据的分类、编码和命名规则,遵循现实世界地理要素的空间关系,建立必要的几何网络和平面拓扑,提供可行的数据安全性策略和有效的数据库备份和恢复机制。     

GIS技术在区域水资源调蓄中的应用——以滹沱河冲洪积扇地下水调蓄研究为例

在对GIS技术进行介绍的基础上阐述了GIS技术在地下水数值模拟中的主要应用;建立了基于GIS的地下水模拟模型,并将其应用于滹沱河冲洪积扇地下水调蓄研究中,调蓄结果表明,研究区现状调蓄空间为29．95×10^8m^3,漏斗区现状调蓄空间为12．83×10^8m^3;采用调蓄方案后,到2020年地下水水位持续下降的趋势得到了缓解和遏制,含水层的储水功能得到了部分恢复和涵养。     

内蒙古大青山地区孔兹岩系中大理岩岩组的地球化学特征及原岩建造

大理岩岩组是内蒙古大青山地区孔兹岩系3个岩组中最上部的一个岩组,该岩组是一套富镁质的大理岩系,以巨厚的、大面积分布的白云质大理岩的发育为特征,底部有少量碎屑岩沉积,矿物组成除白云石外,普遍含蛇纹石化橄榄石、透辉石、金云母等一种或多种富镁硅酸盐矿物。岩石地球化学以富CaO、MgO和LOI为特征,反映了碳酸盐岩的地球化学特征,CaO＋MgO含量达44.96%以上,且CaO/MgO比值较小（1.37～10.94）,其原岩应为一套碎屑含量极低的白云岩,以化学沉积为主。原岩建造的沉积环境：由初期的陆海过渡的三角洲相,过渡到滨海-浅海相,最后到干燥气候条件下有障蔽岛相隔的封闭海盆相。构造环境也从亚稳定状态过渡到稳定构造环境,表明该套变质沉积地层的原岩可能形成于被动大陆边缘,但更类似于中元古界长城系、蓟县系这样的克拉通内裂陷槽或裂谷沉积。     

Geodatabase数据模型驱动的人防地理数据库

为有效地组织人防资源和信息,为人防战时指挥和日常演习提供保障,提出了面向Geodatabase数据模型的人防地理信息系统数据库。该数据库依据地理空间数据标准来确定空间数据的分类、编码和命名规则,遵循现实世界地理要素的空间关系,建立必要的几何网络和平面拓扑,提供可行的数据安全性策略和有效的数据库备份和恢复机制。     

基于数字地球平台的三维虚拟数字校园建设

以虚拟成都理工大学为例,论述了一种高效、低成本的网络虚拟校园建设方法,即利用数字地球平台的基础地理框架和遥感底图,使用建模工具进行三维建筑群模型建立,经过投影和坐标变换处理,实现网络虚拟校园的建设与实施。实验证明,数字地球平台凭借其在丰富资源、网络传输、三维显示等方面的优势,是包括虚拟校园在内的数字工程建设的有效工具。     

Validation of Column-Averaged Dry-Air Mole Fraction of CO_2 Retrieved from OCO-2 Using Ground-Based FTS Measurements

In order to correctly use the column-averaged atmospheric CO_2 dry-air mole fraction(XCO_2) data in the CO_2 flux studies, XCO_2 measurements retrieved from the Orbiting Carbon Observatory-2(OCO-2) in 2015 were compared with those obtained from the global ground-based high-resolution Fourier Transform Spectrometer(FTS) participating in the Total Carbon Column Observing Network(TCCON). The XCO_2 retrieved from three observing modes adopted by OCO-2, i.e., nadir, target, and glint, were separately validated by the FTS measurements at up to eight TCCON stations located in different areas. These comparisons show that OCO-2 glint mode yields the best qualitative estimations of CO_2 concentration among the three operational approaches. The overall results regarding the glint mode show no obvious systematic biases. These facts may indicate that the glint concept is appropriate for not only oceans but also land regions. Negative systematic biases in nadir and target modes have been found at most TCCON sites. The standard deviations of XCO_2 retrieved from target and nadir modes within the observation period are similar, and larger than those from glint mode. We also used the FTS site in Beijing, China, to assess the OCO-2 XCO_2 in 2016. This site is located in a typical urban area, which has been absent in previous studies. Overall, OCO-2 XCO_2 agrees well with that from FTS at this site. Such a study will benefit the validation of the newly launched TanSat products in China.