Early Permian strike-slip basin formation and felsic volcanism in the Manning Group,southern New England Orogen,eastern Australia

The Manning Group is characterised by rapidly filled strike-slip basins that developed during the early Permian along the Peel--Manning Fault System in the southern New England Orogen. Typically, the Manning Group has been difficult to date owing to the lack of fossiliferous units or igneous rocks. Thus, the timing of transition from an accretionary convergent margin in the late Carboniferous to dominantly strike-slip tectonic regimes that involved development and emplacement of the Great Serpentinite Belt (Weraerai terrane) is not well constrained. One exception are rhyolites of the Ramleh Volcanics that were erupted into the Echo Hills Formation. These developed along the dextral Monkey Creek Fault splay east of the Peel--Manning Fault System. Zircons extracted from the Ramleh Volcanics yield a U–Pb (SHRIMP) age of 295.6?±?4.6?Ma that constrains the minimum age of deposition in this basin to earliest Permian. Whole-rock geochemistry indicates these are peraluminous felsic melts enriched in LREE and incompatible elements with strong depletions in U, Nb, Sr and Ti. These are similar in age and composition to the nearby S-type Bundarra and Hillgrove plutonic supersuites. We suggest that extensive movement along the east-dipping Peel--Manning Fault System was responsible, not only for strike-slip basin development at the surface (Manning Group), but was also the locus for crustal melting that was responsible for generating S-type felsic melts that utilised hanging-wall fault splays as conduits to the surface or to coalesce in the crust as batholiths exclusively to the east of the Peel--Manning Fault System.     

台湾东北部地形共振对M2内潮演化影响的数值模拟研究

<正>压潮流、突变海底地形和稳定层结结构是内潮生成的主要因素。台湾东北部海域地形结构多变,正压潮流较强,形成复杂的内潮场。本文通过ROMS(Regional Ocean Modeling System)模式,研究了台湾东北部海域两源区共振条件下内潮的生成、传播和耗散混合过程。结果表明:在台湾东北部海域,Mien-Hua海底峡谷与I-lan海脊是M2内潮重要的生成源区,源区之间的距离与M2内潮水平波长相当,满足共振条件并增强了内潮的生成和耗散。本文通过敏感性试验,探讨模式水平分辨率与不同季节的层化对源区共振过程的影响,数值实验表明,高分辨率的数值模式可以更好地刻画小尺度的地形结构,对复杂地形条件下内潮生成和传播过程的数值模拟十分必要;不同季节的海水层化结构在本质上不改变两源区间的共振关系,但层化强弱对内潮能量的生成具有一定程度的影响。     

Efficient system reliability analysis of rock slopes based on Subset simulation

How to efficiently assess the system reliability of rock slopes is still challenging. This is because when the probability of failure is low, a large number of deterministic slope stability analyses are required. Based on Subset simulation, this paper proposes an efficient approach for the system reliability analysis of rock slopes. The correlations among multiple potential failure modes are properly accounted for with the aid of the “max” and “min” functions. A benchmark rock slope and a real engineered rock slope with multiple correlated failure modes are used to demonstrate the effectiveness of the proposed approach.     

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地震前兆数据库系统设计

基于应用需要, “十五”项目对前兆数据库系统重新进行了统一规划设计, 吸取了此前已有前兆数据库系统的优点, 制定了《地震前兆数据库结构规范 第一部分: 固定台站观测》。 本文详细介绍了该规范设计的有关方面, 包括对此前已有前兆数据库系统的分析、 设计时的考虑因素、 包含的内容、 规范的主要特点、 以及对有关问题的解决, 如同一台站多套相同仪器的处理等。 本文还简要介绍了库表结构, 并与“九五”数据库结构进行了查询速度比较。 基于该结构的前兆数据库系统已在前兆台网的各级节点使用。 实际应用表明, 该数据库结构具有结构稳定、 查询速度快、 表数量和表大小适中、 基础信息全面以及开放性好等优点。     

北斗卫星导航系统在地质调查领域应用综述

北斗卫星导航系统由中国自行研制,拥有完全自主知识产权,具有快速定位、双向通信和精密授时三大功能。介绍了北斗卫星导航系统的特点、功能及其在数据采集与监测、监控与指挥调度等方面的典型应用,总结了北斗卫星系统在野外地质调查与安全保障、地质灾害实时监测、抗震救灾与应急指挥中的应用,重点介绍了基于北斗卫星的野外地质调查服务与管理系统、滑坡实时监测系统、青藏高原地应力实时监测系统、抗震救灾应急指挥系统的组成及功能,并分析了北斗卫星导航系统在地质领域的应用优势。      

捷联惯性导航系统重力扰动影响分析

通过EGM2008地球重力场球谐模型生成某区域重力扰动图,建立重力扰动情况下捷联惯性导航系统误差模型,仿真验证重力扰动的水平分量对捷联惯性导航误差的影响,结果表明：重力扰动的水平分量引起的捷联惯性导航系统的水平位置与速度误差以舒拉周期进行振荡,重力扰动为12.5×10 ^-5 ms ^-2时,位置误差达160 m。     

基于交通、人口和经济的中国城市群识别

城市群是一个国家工业化和城镇化进程发展到较高阶段的自然产物,是国家参与全球竞争与国际分工的新型地域单元。当前,研究人员对城市群的识别尚没有一个统一、快速的技术体系,国内外研究人员对于中国城市群的准确识别和区域界定也不统一。在综合前人研究的基础上,作者首先厘清了城市群的基本概念;继而提出了一套以地球信息技术为支撑的,综合了交通、人口和经济属性判断的城市群快速识别和区划的技术流程,即以空间通达性的定量测算为基础,初步识别出空间上集结的城市集群;然后以城市集群的经济和社会属性为判据开展进一步的遴选,得到城市群空间分布及其区划界线。作者使用基础地理数据、DEM数据、空间化的经济社会格网数据,应用ArcInfo Macro Language 编程技术对中国的城市群进行了识别,研究明确了2000 年中国9 大城市群的空间位置及其覆盖区域。与国内外既有认识的对比表明,本研究技术路线简单、清晰,所得的中国城市群区划成果准确,具有可参比性。