Geochemical characteristics of trace elements and tectonic setting of sandstones from the Upper Ordovician Pingliang Formation,southwestern margin of Ordos Basin: A case study of the Duanjiaxia profile,Longxian County

Due to the lack of reliable sedimentary provenance data,the geological setting and its provenance of the southwestern margin of Ordos Basin in Late Ordovician is uncertain. In this paper,the sandstone of Upper Ordovician Pingliang Formation in Duanjiaxia profile of Longxian area is selected for a systematic study. Using the methods including the comprehensive analysis on the measured geological profile,analysis of microscopic thin section and trace elements,the following results are obtained: (1)the thin section analysis shows that the sandstone is well sorted but poorly rounded. Clastic grains are dominated by quartz,while the rock fragments are mainly composed of polycrystalline quartz,carbonate sand debris,and a little matrix,which means that the turbidite sandstone has been reworked by obvious traction of deep-water;(2)Rare Earth Element(REE)distribution model shows that the sandstone is rich in LREE and is short of HREE and has the negative Eu-anomaly,indicating that the provenance may derive from the intermediate and acid rock in the upper crust;(3)the provenance discrimination diagrams show that the sandstone of the Pingliang Formation is a mixture of sedimentary rock and granite,while the magmatic component is dominated by intermediate and acid rock;(4)Geochemical data of the sandstone suggests that the geological setting significantly belong to continental island arc and passive continental settings. The study area in Longxian during the Late Ordovician period was located in the back arc basin. At that time,the southwestern margin of the North China Craton with the full trench-arc-basin system was changed from the passive continental margin into the active continental margin.     

台湾海峡1998年夏季温盐场的分布特征

根据１９９８年夏季台湾海峡调查所得到的温盐观测资料,分析了该海区的温盐场特征。结果表明：（１）海峡西部主要为低温高盐水分布,而在海峡东部则是受高温低盐水控制。（２）海峡西部表层水体的低温高盐特征反映出深层在台湾海峡不同区域沿陆坡爬升的动力特     

LD2000 System with 3S and Multi—sensor

This paper introduces a car-borne road information collecting and updating system (LD2000) developed by Wuhan Technical University of Surveying and Mapping.This system is capable of collecting road network information and creating digital road network effectively by means of GPS,GIS and multi-sensor integration.The design and development of LD 2000 system are also presented in this paper.     

含双裂隙岩石裂纹演化机理的离散元数值分析

采用离散单元法探讨了预制双裂隙岩石的裂纹演化机理。用近期从试验资料提取的无胶结厚度含抗转动能力的岩石微观力学模型和相应的离散单元法商业软件,模拟了含不同预制倾角的双裂隙岩石试样在单轴压缩作用下裂纹的扩展与贯通规律,揭示了裂纹演化的宏微观机理。同时,将离散元法DEM岩石试样的裂纹的扩展和贯通规律以及强度特性与室内试验结果进行了比较分析。结果表明,预制裂隙之间以及端点处的拉应力集中是导致裂隙岩石破坏的主要原因,且DEM数值试验得到裂纹的演化规律与室内试验结果较为一致。含30°的预制裂隙的岩石试样最容易起裂,含75°的预制裂隙的岩石试样最困难起裂,造成此种现象的原因可能是裂纹在垂直于主应力方向上的长度不同导致试样受拉区域大小不同。     

冀东太平寨紫苏花岗岩类深熔成因的矿物标志

冀东太平寨地区紫苏花岗岩的矿物学研究结果表明,该类岩石中的主要组成矿物具有残晶相和结晶相矿物共存特点。残晶相和结晶相矿物与围岩中同类矿物对比研究表明,该区的紫苏花岗岩类是由其围岩—石英闪长质-英云闪长质紫苏斜长片麻岩深熔而成。     

中国南天山晚石炭世—早二叠世花岗质侵入岩的岩石成因与地壳增生

晚石炭世—早二叠世在中亚南天山造山带形成了大量的花岗质侵入岩.中国境内这些岩体以晚石炭世Ⅰ型花岗岩、早二叠世Ⅰ型和S型花岗岩以及最晚期的A型花岗岩为代表.不同类型的岩石在源区特征和岩浆形成的温压条件上存在一定的差异,而这些差异性反映了该时期内构造环境的演化过程.本文选取铁列克岩体、盲起苏岩体、英买来岩体、川乌鲁杂岩体、...     

频率域电磁测深中的记录规则

首先讨论了频率域电磁测深中的记录规则,然后利用三维数值模拟结果作了具体分析。认为,在不考虑微弱的阴影效应时,将测深点作为频测记录点更为合理。野外试验对比说明了同样的结论。     

大地测量学实践教学改革的探索

大地测量学是测绘工程专业的一门理论性和实践性很强的重要专业基础课。从强化课堂基础实验、重视课程设计、建立生产实习考核体系等3个方面提出了实践教学改革措施,在帮助学生巩固加深理论知识,提高学生运用知识分析解决问题的能力和实践创新能力等方面具有重要的意义。     

Palaeoseismic records in lacustrine sediments—A case study of the Daqingshan piedmont fault and Hasuhai Lake in Inner Mongolia,China

As a traditional method for palaeoseismic studies, trenching can be combined with dating techniques to identify palaeoseismic events and the earthquake recurrence interval. However, when using trenches to study palaeoearthquakes, factors such as the active tectonic background of the earthquake‐caused structure, the lithology on both sides of the fault, the geomorphology location and type and the samples and methods for dating will affect the location of the trench. Thus, trenches should be carefully selected and used to identify the impact of ancient earthquakes. The results have substantial uncertainties and limitations. In recent years, scholars have made considerable progress in using other methods to reveal the palaeoseismic information of faults. Moreover, the history of fault activity may have been recorded in the lacustrine sediment adjacent to the fault. Hasuhai Lake is adjacent to the middle segment of the Daqingshan piedmont fault in Inner Mongolia. Since the Holocene, the region has experienced a temperate continental semi‐arid climate with little interference, and Hasuhai Lake and peripheral waters present weak hydrodynamic conditions that provide an ideal location for the study of palaeoseismic records in lacustrine sediments. Sediment samples and samples for dating were collected from three trenches excavated on the periphery of the Hasuhai Lake. Their variations in grain size and magnetic susceptibility revealed that wind and flowing water jointly produced the sedimentary conditions of Hasuhai sediments. The ¹⁴C dating results and variations in the grain size distribution, grain size components and magnetic susceptibility of sediments caused by seismic events obtained in this study were compared with those caused by a series of palaeoseismic events at the middle segment of the Daqingshan piedmont fault reported by previous studies using trenches, knickpoints and palaeosol records. The results identified seven palaeoseismic events recorded near Hasuhai Lake since 12,000 years. The combined use of lacustrine sediment variation characteristics and dating techniques is an effective method for studying palaeoseismic events.