利用瑞利面波相速度和方位各向异性研究鄂尔多斯块体的岩石圈变形特征   总被引：1，自引：1，他引：0       下载免费PDF全文

姚志祥  王椿镛  Eric Sandvol  陈永顺  曾融生 《地球物理学报》2014,57(9):2777-2789

利用在鄂尔多斯块体内部布设的45个宽频带流动台站和固定台站的资料,用双平面波方法反演了20~143 s共12个周期的基阶瑞利面波的平均相速度和方位各向异性,并反演了一维S波速度结构.反演结果显示50~100 s中长周期的瑞利面波相速度高于AK135速度模型的相速度,为高速异常,S波速度显示高速异常主要位于180 km深度范围内,表明鄂尔多斯块体保留有厚的高速岩石圈.20~111 s周期的方位各向异性强度小于1%,较小的各向异性表明鄂尔多斯块体岩石圈变形较弱.20~50 s周期的平均快波方向为近EW向,67~143 s周期的平均快波方向为NW-SE向,相对发生了整体改变,快波方向的转变约开始于80~100 km深度范围,这表明岩石圈上下部存在着由不同变形机制导致的各向异性.上部岩石圈中各向异性可能主要为残留的“化石”各向异性,而下部岩石圈各向异性可能是现今板块构造运动导致的变形而形成.鄂尔多斯块体岩石圈垂向上的变形差异可能主要与岩石圈温度随深度的变化以及青藏高原NE-NNE向挤压引起的上部岩石圈逆时针旋转有关.  相似文献   

Interferometry basics in practice: Exercises     

Florentin Millour  Damien Sgransan  Jean-Philippe Berger  Gilles Duvert  Fabien Malbet 《New Astronomy Reviews》2008,52(2-5):208

The following exercises aim to learn the link between the object intensity distribution and the corresponding visibility curves of a long-baseline optical interferometer. They are also intended to show the additional constraints on observability that an interferometer has.This practical session is meant to be carried out with the ASPRO software, from the Jean-Marie Mariotti Center, but can also be done using other observation preparation software, such as viscalc from ESO.There are two main parts with series of exercises and the exercises corrections. The first one aims at understanding the visibility and its properties by practicing with simple examples, and the second one is about UV coverage.  相似文献   

All you ever wanted to know about optical long baseline stellar interferometry, but were too shy to ask your adviser     

Florentin Millour   《New Astronomy Reviews》2008,52(2-5):177

I try to present a small view of the properties and issues related to astronomical interferometry observations. I recall a bit of history of the technique, give some basic assessments to the principle of interferometry, and finally, describe physical processes and limitations that affect optical long baseline interferometry and which are, in general, very useful for everyday work. Therefore, this text is not intended to perform strong demonstrations and show accurate results, but rather to transmit the general “feeling” one needs to have to not be destabilised by the first contact to real world interferometry.  相似文献   

去均值归一化互相关最小二乘逆时偏移及其应用   总被引：1，自引：1，他引：0       下载免费PDF全文

李庆洋  黄建平  李振春  李娜  李闯 《地球物理学报》2016,59(8):3006-3015

最小二乘逆时偏移相对于常规逆时偏移具有更高的成像分辨率、振幅保幅性及均衡性等优势,在一定程度上可满足岩性油气藏勘探的需求,是目前研究的热点之一.然而由于实际地下介质的黏滞性和变密度,以及无法准确地估计震源子波等,基于振幅匹配的常规最小二乘逆时偏移算法很难在实际资料处理中取得好的效果.此外,实际数据常包含大量噪声,进一步限制了常规算法的应用.为此,本文通过修改目标泛函,提出了去均值归一化的互相关最小二乘逆时偏移算法,并给出了陆上资料的应用实例.研究表明,归一化策略减弱了算法对子波能量的苛求;互相关算法强调相位匹配,进一步弱化了子波的影响,提升了算法的稳定性和可靠性;去均值思想在处理低信噪比资料方面有较大优势.理论模型和陆上实际资料处理都验证了本算法的有效性和对复杂模型的适应性.  相似文献   

The solar and lunar effect of earthquake duration and distribution     

Zhenxia Zhang  Shugui Wu  Jianyong Li 《地震科学（英文版）》2013,26(2):117-124

Phase folding algorithms are conventionally used in periodicity analyses using X-ray astronomy pulsar. These allow for accurate identification of the cycle and phase characteristics of the physical parameters of the periodic variation. Although periodic variations in earthquake activity have long been studied, this paper is the first to apply the phase folding algorithm to the analysis of shallow (<70 km) seismic data for the period 1973–2010. The goal is to study the phase distribution characteristics of earthquake frequencies and we see a connection between earthquake occurrence and solar and lunar cycles. First, the rotation of the Sun may play a significant role in impacting on the occurrence time of earthquakes with magnitudes of less than 6.0. This may be especially pertinent for earthquakes with magnitudes between 5.0 and 6.0, when the modulation ratio reaches 12 %. The Moon’s gravity, which is generally thought to have the greatest influence on the global environment, may actually play less of a role on earthquake timing than the rotation of the Sun. Second, when we consider the world to be divided into 72 local regions based on latitude and longitude, we can see that there are more than a dozen regions with significant non-uniform distributions of earthquake occurrence time. In these regions, the ratio of χ ² to the number of degrees of freedom far exceeds five. As a result, we posit that some factors associated with the Sun–Earth–Moon relationship may trigger earthquake activity under certain temporal and spatial conditions.  相似文献   

利用多台资料对比识别南北地震带震相特征     

杨广华  白香玲 《高原地震》2008,20(1):7-13

利用多台资料对比震相识别方法,采用台网中心对地震较精确的定位结果,对南北地震带强化观测台网中心所记录到的地方震、近震、远震分别进行分析。结果表明,随着不同构造区域介质的差异性,地震波传播路径不同,导致各地区所记录到的地震震相特征不同。通过对不同区域地震震相特征的进一步对比分析,找出各区域震相特征的差异性和规律性,为以后台网中对震相识别和精确定位都有一定意义。  相似文献   

GPS扼径圈天线相位中心偏差检验     

赵永年  王建华  师昭梦  王雄 《高原地震》2008,20(1):52-56

GPS接收机天线相位中心偏差是指GPS天线接收卫星信号的电气中心与其机械几何中心之差,在GPS高精度测量中,这是不容忽视的。讨论了采用基线测量相对定位法确定天线相位中心偏差的原理和方法,并利用这一方法计算出天线相位偏差结果。  相似文献   

Metamorphism and exhumation of basement gneiss domes in the Quadrilátero Ferrífero:Two stage dome-and-keel evolution?     

Kathryn Cutts  Cristiano Lana  Fernando Alkmim  Federico Farin  Hugo Moreira  Viviane Coelho 《地学前缘(英文版)》2019,10(5):1765-1787

The presence of dome-and-keel provinces in Archean cratons has been connected with the initiation of plate tectonics on Earth as these features are most commonly observed in Archean rocks.The Quadrilátero Ferrífero in Brazil has been identified as a Paleoproterozoic dome-and-keel province for more than three decades.The prevailing model suggests that it formed during the Rhyacian Transamazonian orogeny,making it unique among dome-and-keel provinces.However,a lack of appropriate lithologies,datable minerals and the metamorphic overprint of later orogenesis has resulted in a cryptic metamorphic record for the formation of this dome-and-keel province.A clinopyroxene-bearing migmatite from the core of the Ba??o dome has peak P-T conditions of 5-7 kbar and 700-750 ℃ and a published age of ca.2730 Ma based on U-Pb ages of zircon from leucosomes,suggesting that this age represents the migmatisation event.A fine-grained epidote-albite-titanite assemblage overprints the coarse-grained clinopyroxene and amphibole,giving P-7 conditions of 8-9 kbar and 550 ℃ with an associated titanite age of ca.2050 Ma.A garnet-bearing amphibolite sample also from the core of the dome has peak P-T conditions of 7-8 kbar and 650-700 ℃,and texturally late titanite from this sample produces an age of ca.2060 Ma.Three additional samples were collected from the edges of the dome.A garnet-gedrite bearing felsic schist produces peak P-T conditions of 8-9 kbar and 650-700℃ on a clockwise P-T evolution.This sample has a U-Pb zircon age of ca.2775 Ma,which could date metamorphism or be the age of its volcaniclastic protolith.Texturally unconstrained titanite from the sample gives an age of ca.2040 Ma.A garnet-bearing amphibolite that occurs as a boudin within the felsic schist gives both zircon and titanite ages of ca.2050 Ma and has peak P-T conditions of 5-6 kbar and 650-700 ℃ on a near isobaric P-T path.An amphibolite dike,observed to cross-cut the felsic schist produces a zircon U-Pb age of ca.2760 Ma.Altogether this data suggests that the samples were metamorphosed in the Archean(ca.2775-2730 Ma)and again during the Transamazonian event.The most plausible explanation for this data is that dome-and-keel formation occurred in the Archean with migmatisation and high-temperature metamorphism occurring at this time.The Paleoproterozoic event is interpreted as a reactivation of the dome-and-keel formation structures,with Paleoproterozoic keels crosscutting Archean keels and producing metamorphic aureoles.The high radiogenic heat production and the presence of dense sedimentary successions in Archean terranes make dome-and-keel provinces a uniquely Archean feature,but they are susceptible to reworking,resulting in an enigmatic record of formation.  相似文献   

Origin和Matlab软件在水盐体系相图绘制中的应用   总被引：1，自引：0，他引：1       下载免费PDF全文

刘元会  邓天龙  宋彭生 《盐湖研究》2008,16(1):36-41,72

随着Origin和Matlab等计算机软件应用于相图的绘制,相图的绘制将更加简洁准确,并可形成数字化相图。介绍了Origin软件在水盐体系平面相图绘制和Matlab软件在水盐体系立体相图绘制中的应用,指出了两种软件在相图绘制中尚待改进的功能。  相似文献   

三元体系NaCl-CaCl2-H2O 25℃相关系研究   总被引：1，自引：0，他引：1       下载免费PDF全文

丁秀萍  毕玉敬  时历杰  宋彭生  孙柏 《盐湖研究》2009,17(3)

采用等温溶解平衡法,研究了三元体系NaCl-CaCl2-H2O 25℃时的溶解度,确定了该体系共饱点的组成,共饱点液相组成是NaCl 0.75%,CaCl244.99%、H2O 54.26%。对应的平衡固相为CaCl2.6H2O和NaCl。两种原始组分未形成复盐或固溶体,体系属于简单共饱型。  相似文献