Crustal velocity structures and their tectonic implications in different tectonic block regions of the Chinese mainland     

Xiankang Zhang Yonghong Duan Jinren Zhao Chengke Zhang Shixu Jia Jianshi Zhang Fuyun Wang Zhuoxin Yang  Suzhen Pan Geophysical Exploration Center  China Earthquake Administration  Zhengzhou  China 《地震学报(英文版)》2009,(4):337-346

In this paper,the typical velocity structures and average velocities of the crust in six different active tectonic block regions are presented on the basis of previous studies and their tectonic implications are discussed. The results show that different tectonic units have different features of crustal velocity structures. In general,there are low velocity distributions in the crust in regions with strong tectonic activities,and the scales of low velocity distributions are related to the tectonic activitie...  相似文献   

FZY-1型多分量式钻孔应变仪的设计     

李海亮  马鸿钧  张钧  李秀环  马相波  周佩侠  苏恺之 《地震地磁观测与研究》2004,25(1):69-77

介绍了最新研制的FZY-1型多分量式钻孔应变仪的探头的设计,所采用的电路,仪器参数的检测方法及该仪器的安装方法。  相似文献   

黄河小浪底斜坡变形的“反迭瓦”式构造机制研究     

王宝军  李清波 《高校地质学报》1999,5(1):100-104

针对小浪底地区斜坡中普遍发育的“返迭瓦”式构造,结合该区的工程地质条件,对其成因机制进行分析。提出了“反迭瓦”式构造的形成是由于边坡蠕变形的结果,并非造成滑坡的原因。  相似文献   

Experimental Research on Shear Behavior of Reinforced Concrete Composite Beams Under Uniformly Distributed Load     

ZHAO Shunbo Ass. Prof.  North China Institute of Water Conservancy  Hydroelectric Power  Zhengzhou  P. R. China. 《中国海洋工程》1998,(4)

An experimental program was carried out to study the shear behavior of the reinforced con-crete composite beam(RCCB)subjected to two-phase uniformly distributed load.A total of 12 reinforcedconcrete composite beams were tested:10 of them were the RCCB subjected to two-phase uniformly dis-tributed load,the other 2 were the comparative reinforced concrete beams cast at the same time as theRCCB subjected to one-phase uniformly distributed load.The interface of precast unit and recast concretewas natural and rough.The test range of the main composite factors:the ratio of precast section depth tocomposite section depth was from 0.35 to 0.65,the ratio of first-phase load moment to precast section ulti-mate bearing moment was from 0.25 to 0.65.Based on the test results,the stresses of the longitudinal rein-forcements and stirrups,the load-bearing properties of the interface,the crack state and the failure charac-teristics of the RCCB under uniformly distributed load are discussed.The effects of the stirrups,the  相似文献   

对"地幔对流"的几点质疑     

池顺良  骆鸣津 《大地测量与地球动力学》2003,23(2):107-110

地幔对流被认为是板块运动的驱动力源，但板块说提出35年来，始终未能阐明地幔对流是如何推动板块运动的，也未能证明地幔对流的存在。相反，却有观测与实物证据证明地幔对流并不存在。对地幔对流提出的质疑与剖析，将有助于地球动力学研究思路的扩展。  相似文献   

Two-step interface and velocity inversion—— Study o e of the Tangshan seismic region     

XIAO LING LAI XIAN KANG ZHANG XU YAO ZHENG Research Center of Exploration Geophysics  China Seismological Bureau  Zhengzhou  China 《地震学报(英文版)》1998,(6)

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徐君毅  曾安敏 《大地测量与地球动力学》2009,29(5):116-120

???????????????????????????????????????ARIMA???????????????????????1?????????????????????????????з???????????????????????β???????????????????????MA????????????????????????ARIMA??0??2??q?????????????????????????ARIMA??0??2??q?????????????????????ζ?????????????  相似文献   

利用小波变换方法分析跨断层形变异常   总被引：16，自引：8，他引：8  

李杰  李明海  刘希强  张京华  郑树田  范军 《大地测量与地球动力学》2004,24(3):73-78

为了从跨断层形变观测资料中获取中强地震的前兆异常信息，运用二进小波变换方法和噪声与信号的定量识别方法，分析了不同尺度的小波变换的细节信号变化特征。研究结果表明：(1)不同尺度小波变换分解的细节信号显示出不同的时变特征。当尺度为1时。细节信号主要为噪声；尺度为2、4、5时，细节信号主要为非平稳信号；尺度为3时，细节信号主要为平稳周期信号；(2)每月观测一次的跨断层形变资料在尺度为3时的细节信号有较好的年周期特征；(3)当尺度为3时的细节信号变化超出2倍均方误差时，测点周围200km左右范围内发生中强地震的可能性很大。  相似文献   

Recently Ratified and Proposed Cambrian Global Standard Stratotype-section and Points     

PENG Shanchi  ZHU Xuejian  ZUO Jinxun  LIN Huanling  CHEN Yong’an  WANG Longwu 《《地质学报》英文版》2011,85(2):296-308

This paper briefly summarizes an officially ratified Global Standard Stratotype-section and Point (GSSP) and a proposed GSSP for global stages of the Cambrian System. The Luoyixi section near Luoyixi town, Guzhang, northwestern Hunan is ratified as the boundary stratotype for the base of the global Guzhangian Stage, which is the upmost stage of an unnamed series termed provisionally as Cambrian Series 3. The GSSP position lies 121.3 m above the base of the Huaqiao Formation in the section, coinciding with the first appearance of the cosmopolitan agnostoid trilobite Lejopyge leavigata. The Duibian B section at Duibian village, Jiangshan, western Zhejiang, is proposed as the boundary stratotype for the base of the proposed global Jiangshanian Stage that is the second stage of the Furongian Series. The proposed GSSP position lies 108.12 m above the base of the Huayansi Formation in the section, coinciding with the first appearance of the cosmopolitan agnostoid trilobite Agnostotes orientalius. This horizon is also with the first appearance of the cosmopolitan polymerid trilobite Irvingella angustilimbata.  相似文献   

岩浆热液成矿理论的失败:原因和出路   总被引：8，自引：0，他引：8  

罗照华  卢欣祥  刘翠  李德东  杨宗锋  文思博 《吉林大学学报(地球科学版)》2011,41(1):1-11

流行的岩浆热液成矿理论假定含矿流体由岩浆分异作用、特别是分离结晶作用产生。由于大型、超大型矿床往往与小岩体有关,而小体积岩浆不能满足质量平衡的要求,其支持者进一步假定含矿岩体的深部存在一个大岩浆体。这种解释与矿区观察到的地质现象和理论推导结果相悖:(1)含矿斑岩中常见暗色微粒包体和大量具有较高密度的矿物,表明岩浆没有发生分离结晶作用;(2)流体的活动性远大于硅酸盐熔浆,没有证据表明岩浆分异产生的流体要在熔浆固结之后才开始活动;(3)矿区普遍见有同成矿的宽谱系岩墙群,暗示成矿期不存在大的深部岩浆房。因此,岩浆热液成矿理论遭遇的困境不仅仅是质量平衡问题,有必要重新思考岩浆相关矿床的形成机制。岩浆热液成矿理论失败的深层原因则是它将成矿作用看作是理想系统中的平衡线性过程,而成矿系统实际上是一种复杂性动力系统,成矿作用是一种非平衡、非线性过程;换句话说,在流行的岩浆热液成矿理论中,对成矿系统和成矿作用的基本属性缺乏正确的理解。在当今科学发展水平上,其失败是必然的,因而有必要构筑新的成矿理论。依据复杂性科学的基本原理,罗照华等(2007,2009)将熔浆和含矿流体看作是成矿系统中2个独立的子系统,认为它们的强相互作用及其环境约束主导了成矿系统的戏剧性变化;进而构筑了一个新的框架性模型,称为透岩浆流体成矿理论。该理论不仅可以解释比流行岩浆热液成矿理论更多的地质现象,还可以推导潜在的具体找矿标志,可能成为岩浆相关矿床成因研究的新起点。  相似文献