黄河中游新近系红粘土粒度特征及其古环境——以陕西府谷老高川为例

黄河中游新近系红粘土粒度分布表现出明显的三峰分布，说明它是由多种成因组份构成，而且每种成因组份对整体的贡献率也不同。其粒度组成主要是以粉土粒级(5～50μm)为主，而250μm以上的颗粒少见。除小于1μm和小于2μm粒级含量变化相对稳定外，其余粒级均表现出旋回起伏的特征。大于63μm和大于30μm及中值曲线变幅较大，说明当时冬季风比较盛行，而且变化强度比较大；而小于2μm粒级曲线变化相对稳定，说明当时夏季风很弱，而且没有太大变化。粒度曲线与野外岩性所得结论相一致，说明当时气候总体上是以干冷为背景，但也有干冷与暖湿的交替。野外岩性上表现为粘土层与钙结核层相互交替，粒度曲线上表现为峰谷旋回起伏的变化，同时也有古生物证据与岩石学证据相佐证。     

岩浆岩成因类型REE判别

本文根据REE丰度特征与对数真数特征的关系以及REE燕式曲线的物理定义 (化学内涵 )和数学关系 ,引入了丰度坐标系———双对数坐标系 (一种准四维坐标系 )定量模型 ,按照岩浆岩系的数据点在丰度坐标系中的分布情况 ,对岩浆岩系REE丰度结构进行分类 ,并探讨岩浆岩系的REE演化类型和演化运动特征 ,据此对岩浆岩成因的类型进行判别     

阻滑桩加固土坡稳定性分析的上限解法

从极限分析机动学方法出发,利用土的抗剪强度折减系数概念,建立了土坡的极限平衡状态方程,由此确定土坡的临界稳定安全系数及其相应的潜在破坏模式.对于典型问题,通过与现有极限平衡解和有限元数值解的对比分析,验证了这种上限解法的合理性.进而对于在给定的荷载条件下不能满足抗滑稳定性要求的土坡,考虑采用阻滑桩加固方式,根据桩侧有效土压力的合理分布模式确定桩体与滑动面相交的截面上等效抗滑力和抗滑力矩,利用极限分析上限定理建立了阻滑桩加固土坡的极限平衡状态方程,将桩侧土压力作为目标函数,运用数学规划方法确定了极限平衡状态时的临界桩侧土压力,以此为土坡加固中阻滑桩设计提供依据.通过数值计算与分析探讨了阻滑桩加固位置的优化布置等问题.     

遥感变化检测技术发展综述

卫星遥感的复轨能力，稳定一致的传感器参数和系列运行计划，连续记录了地表的显著变化信息。对遥感观测到的变化信息，还需要区分是地表物理生物要素变化引起的变化，还是辐射传输路径上其它干扰因素造成的变化信息，需要从各种变化信息组分中区分目标变化信息。因此，遥感变化检测是遥感信息科学、地球系统科学、统计学和计算机技术等学科技术交叉后新的增长点，代表了当前遥感数据处理技术发展方向。为了促进遥感变化检测技术在我国的发展，收集阅读了近几年国外主要遥感刊物发表的论文、专著，综合了我国遥感变化检测技术发展现状以及大量的网络资料。     

Spectral Representation and Analysis of the KBR Precision Based on the Earth Gravity Spectrum

IntroductionThe GRACE (gravity recovery and cli mate ex-peri ment) mission,twin satellites flying in for-mation ,which carries several key payloadsinclu-ding KBR (K-band ranging) system, waslaunchedin 2002 . The unique design of GRACEmissionis expected to lead to ani mprovement inseveral orders of magnitude in these gravitymeasurements and allow much i mproved resolu-tion of the Earth gravity field of finer scale overbothland and ocean to study a lot of geosciencesphenomena[1]. Though th…     

印度洋9.0级大地震激发的基频地球球型振荡

分析了中国数字地震台网（CDSN）改造后的余山台（SSE）甚长周期地震仪（STS-1，瑞士生产）观测到的大地震后3天的VHZ波形资料，利用功率谱密度估计方法，在没有对资料进行去固体潮处理的情况下，准确获得了2004年12月26日印度洋地震激发的基频球型振荡，并与地球初步参考模型（PREM）的理论自由振荡周期进行了对比，发现实测振荡周期与PREM预测的振荡周期其本符合。其细微差异可以用来研究和解释地球介质的横向不均匀性和各向异性等现象。     

Overbank deposition along the concave side of the Red River meanders,Manitoba, and its geomorphic significance

Slow earth sliding is pervasive along the concave side of Red River meanders that impinge on Lake Agassiz glaciolacustrine deposits. These failures form elongated, low‐angled (c. 6 to 10°) landslide zones along the valleysides. Silty overbank deposits that accumulated during the 1999 spring freshet extend continuously along the landslide zones over hundreds of metres and aggraded the lower slopes over a distance 50 to 80 m from the channel margin. The aggradation is not obviously related to meander curvature or location within a meander. Along seven slope profiles surveyed in 1999 near Letellier, Manitoba, the deposits locally are up to 21 cm thick and generally thin with increasing distance from, and height above, the river. Local deposit thickness relates to distance from the channel, duration of inundation of the landslide surface, mesotopography, and variations in vegetation cover. Immediately adjacent to the river, accumulated overbank deposits are up to 4 m thick. The 1999 overbank deposits also were present along the moderately sloped (c. 23 to 27°) concave banks eroding into the floodplain, but the deposits are thinner (locally up to c. 7 cm thick) and cover a narrower area (10 to 30 m wide) than the deposits within the landslide zones. Concave overbank deposition is part of a sediment reworking process that consists of overbank aggradation on the landslide zones, subsequent gradual downslope displacement from earth sliding, and eventually reworking by the river at the toe of the landslide. The presence of the deposits dampens the outward migration of the meanders and contributes to a low rate of contemporary lateral channel migration. Concave overbank sedimentation occurs along most Red River meanders between at least Emerson and St. Adolphe, Manitoba. © Her Majesty the Queen in right of Canada.     

Paleomagnetic results of the Cretaceous marine sediments in Tongyouluke, southwest Tarim

Southwest Tarim (hereafter SW Tarim) is one of afew areas that well developed Cretaceous marinesedimentary rocks in China [1]. The Cretaceous marinesediments are stretched in front area along the Tian-shan and Kunlun Mountains. Toward the center ofTarim Basin, the Cretaceous sediments are buried bygreat thickness of Tertiary and Quaternary sedimentswith little exposure. Compared with the Cretaceousterrestrial strata of north Tarim, the Cretaceous marinestrata of SW Tarim continue and d…     

“白垩纪大洋红层——海洋/气候响应”研究进展综述

“白垩纪大洋红层”是中国学者提出并开拓的白垩纪研究新方向。在其所领导的两个国际地质对比计划项目(IGCP463/494)的推动下,“白垩纪大洋红层”所蕴含的古海洋与古气候意义,正引起越来越多的学者的重视。特别是近几年召开的学术会议对“白垩纪大洋红层”研究起到了很好的推动作用: (1)在2002 年度IGCP463 项目启动会议上,对“白垩纪大洋红层”的研究现状进行了初步的交流,制订了项目研究的总体目标和未来五年工作计划,并考察了亚平宁—阿尔卑斯—喀尔巴阡沿线的大洋红层;(2)2003 年度的IGCP463 工作会议和IGCP494 启动会议,不仅积累了大洋红层研究的资料,而且将白垩纪大洋红层研究推进到白垩纪中期;(3)2004 年度两个项目的工作会议,以及通过在第32 届国际地质大会特别讨论会的工作,进一步推进了大洋红层的研究,并将“白垩纪大洋红层”研究介绍给广大的国际地球科学界;(4)在欧洲地球科学联盟2005 年会上,“白垩纪大洋红层”研究体现出了多学科共同参与的可喜现象。回首近几年来的研究历程可以发现,“白垩纪大洋红层”研究已实现了如下转变:(1)从区域性研究到全球对比综合研究的变化;(2)从由中国科学家单独研究变为多个国家的科学家申请到项目和经费共同研究;(3)从举办IGCP项目学术年会快速向国际大会或     

On the Progress Design of Integrated Geologic Analysis System: Object-Relational Database Model and Visualization for Earth Resources

Abstract. An object-relational data model is an entry point and integral part of geologic analysis system, in which we can start geologic modeling inside a database. A conceptual data model named the Geoscience (Earth Resources) Data Model 3.0 has been developed based on the conceptual design of NADM-C1.0 and EGDM 812. Such adaptation makes this data model interoperable with data models from other geoscience fields. The focus of current data model is to effectively manage multi datasets related with the study of earth resources and to create relationship among data types.
The conceptual data model for earth resources is successfully implemented physically by integrating a GIS and relational data storage. The direct link between relational database and GIS makes the database contents highly visual and spatially enabling. Database contents are fully georeferenced through different types of georeferencing systems that enables data integration, visualization and analysis of multi geoscience datasets in 2D and 3D environment. A new way of geologic analysis through visualization of virtually all kinds of geoscience datasets is proposed.
The earth resources research and industry can take benefits on this system through better data management and effective geologic visualization that in turn accelerate a better understanding of earth resources. Meanwhile wider geoscience community will benefit from better interaction and data sharing among geoscience fields for accelerating a better understanding of our complex earth.