Structural Characteristics of the Andaman Forearc Inferred from Interpretation of Multichannel Seismic Reflection Data

The Andaman Forearc Basin(AFB) is asymmetric in configuration and filled with a ~6 kmthick pile of Neogene to Recent sediments(~4 s in two-way travel time:TWT) with distinct zonation.It shows gradual thinning up to ~3 km(0.8 s in TWT) towards the eastern end with a seabed gradient of 1:30.Thick deformed sediments ~2 s(TWT) of the Outerarc are associated with intense faulting and occasional folding caused by recent tectonics.Development of a series of faults within the upwarped sedimentary column of Oligocene top to Recent is observed with a rotated fault block.These features are manifestations of Recent igneous intrusion,and reveal the presence of a mild N–S compressional regime.Its effect on the AFB resulted in further uplift of sediments,which can now be seen as the Invisible Bank.Forward gravity modelling supporting our seismic interpretation reveals that it is associated with igneous intrusion from the Moho(~9 km depth),and also suggests that continental crust underlies the AFB.Strong Bottom Simulating Reflector(BSR)-like features in the Miocene sediments of Outerarc and Forearc basin at a depth of 0.6 s below the seabed suggest the inferred probable occurrence of gas hydrates in the AFB.     

国土资源部、广西壮族自治区岩溶动力学重点实验室2015年开放研究课题申请指南

国土资源部、广西壮族自治区岩溶动力学重点实验室依托于中国地质科学院岩溶地质研究所,主要研究方向：（1）岩溶动力系统的形成和运行规律;（2）岩溶动力系统的类型和区域分布规律;（3）学科交叉、应用研究。2014年在广西科学技术厅和岩溶地质研究所的支持下设立开放课题,围绕岩溶动力系统与全球变化、岩溶地区水循环、岩溶生物地球化学循环过程及相关测试应用技术开展研究。     

磁赤铁矿对有机染料吸附行为的特征研究

利用标准地质样品磁赤铁矿,运用XRD,BET对其进行晶型及比表面积的表征。采用动态吸附实验,研究了磁赤铁矿对浓度为1.0×10-5 mol/L的酸性桃红(Sulforhodamine,SRB),结晶紫(Crystal violet,CV)的吸附特性。考察了溶液离子浓度、pH、吸附时间以及吸附剂投加量对其吸附特性的影响。结果表明,在相同实验条件下,SRB在100min达到吸附平衡,CV在20min达到吸附平衡。溶液pH和离子强度对其吸附都有很大的影响,磁赤铁矿对CV及SRB的最大吸附量分别为3.27×10-3及0.587×10-3。利用Langmuir和Freundlich等温吸附模型对吸附过程进行描述,结果表明,磁赤铁矿对SRB的吸附符合Freundlich模型,对CV的吸附属于Langmuir模型。用准一级和准二级吸附动力学方程对实验数据进行了线性回归分析,结果表明SRB属于准一级动力学方程,CV属于准二级动力学方程。热力学研究表明,磁赤铁矿吸附CV及SRB的过程都是自发进行的吸热反应。     

不同类型烷基铵在蒙脱石中的吸附动力学特性

蒙脱石/烷基铵改性产物是一种重要的高附加值矿物材料,蒙脱石对烷基铵的吸附特性决定所制备的改性产物在各类溶剂体系中的凝胶性能和应用特性。本文以两种层电荷不同的膨润土为原料,在提纯、钠化的基础上,系统研究了80℃恒温条件下十八烷基三甲基铵(OTAC)、十六烷基三甲基铵(CTAC)及十四烷基三甲基铵(TTAC)在两种蒙脱石上的吸附动力学特性。研究结果表明:80℃的恒温条件下,烷基铵插层剂的浓度对等温吸附进程影响显著。当三种烷基铵用量较低(1.0CEC)时,在5min左右就可以达到饱和吸附;当烷基铵用量较高(2.0CEC)时,在30min~60min可以达到饱和吸附;两种蒙脱石对三种烷基铵吸附动力学数据均符合准二级反应动力学方程,相应三种烷基铵在两种蒙脱石中平衡吸附量的实验值和计算值qe基本相等;交换液中烷基铵浓度高低对吸附反应的速率常数影响显著,烷基铵在低用量(1.0CEC)下在蒙脱石中的吸附反应速率常数明显高于其在较高用量(2.0CEC)下的吸附反应常数;烷基铵在高层电荷Na-HLCM中的吸附反应速率常数总体上较低层电荷Na-HLCM的略高。     

遥感新书启事

正继《地球的圆涌构造与深源强爆热动力学》之后,陈荫祥就宇宙-地球强动力的研究新成果编著出《核动力地球学》一书。该书在遥感地球动力学和宇宙超强动力学探索方面有新的进展,希望能为拓展遥感应用提供理论引导和专业科技参考。目前,该书已由现代文化出版社出版。书号:ISBN 978-988-12887-3-8咨询电话:13521512608     

基于某无人机平台的测云雷达结构动力学分析

采用有限元方法对装载于某无人机平台的测云雷达结构进行动力学分析研究。针对具体的机载平台讨论振动环境对雷达结构的影响,依据GJB150.16计算振动的加速度功率谱密度值,并以此为有限元分析的输入,进行雷达结构的模态分析、随机振动分析,又依据GJB150.18中的激励波形进行冲击响应分析,得到结构的应变及应力响应,为该型无人机载测云雷达总体结构的刚强度设计提供了重要的理论依据。     

Jason-2卫星星载GPS数据cm级精密定轨

Jason-2卫星为测高卫星,需要cm级的轨道精度。利用Jason-2星载GPS数据,采用简化动力学法进行了Jason-2卫星精密定轨。对简化动力学轨道进行重叠轨道对比,径向精度达到1.19cm;与CLASS提供的POE结果对比,径向精度达到5.54cm;与SLR数据进行对比,整体精度达到6.63cm。因此,简化动力学轨道达到了cm级要求,定轨精度良好。     

星际甲醇（CH3OH）脉泽

简要综述了近年来对于星际ＣＨ３ＯＨ脉泽的观测和研究成果，对ＣＨ３ＯＨ脉泽的性质从分类，生成区域及分布，辐射特性，运动状况等方面做了介绍，并阐明了理论上对其时变特性，激发机制及河外脉泽的探讨，最后对两种类型的ＣＨ３ＯＨ脉泽作了对比和讨论。     

Earthquake, strong tide and global low temperature

＂La Madre＂ is a kind of upper atmospheric air current, and occurs as ＂warm phase＂ and ＂cold phase＂ in the sky of Pacific Ocean alternately. There exists this phenomenon, called ＂Oscillation Decade in the Pacific＂ （ODP）, for 20 - 30 years. It is concerned with 60 year cycle of the tides. Lunar oscillations explain an intriguing 60-year cycle in the world＇s temperature. Strong tides increase the vertical mixing of water in the oceans, drawing cold ocean water from the depths to surface, where it cools the atmosphere above. The first strong seismic episode in China was from 1897 to 1912; the second to the fifth was the in 1920-1937, 1946-1957, 1966-1980, 1991-2002, tsrectruely. The alternative boundaries of＂La Madre＂ warm phase and cold phase were in 1890, 1924, 1946 and 2000, which were near the boundaries of four strong earthquakes. It indicated the strong earthquakes closedly related with the substances＇ motion of atmosphere, hydrosphere and lithosphere, the change of gravity potential, and the exchange of angular momentum. The strong earthquakes in the ocean bottom can bring the cool waters at the deep ocean up to the ocean surface and make the global climate cold. the earthquake, strong tide and global low temperature are close inrelntion for each othen.     

天文动力学和天体力学

叙述了与Astrod工程有关的天体力学和天文动力学的基本结果和学科概况 ,内容包括二体问题、摄动理论、人造地球卫星运动、限制性三体问题等