断裂应力场模拟分析与应用

采用岩石破坏过程分析系统 (RFPA2D) ,通过对断裂应力场数值模拟分析 ,表明构造应力场条件下含断裂岩体的声发射的能量最大值和累计值都远大于重力场 ,说明构造应力场条件下岩体应力大大高于重力场 .通过对北票矿区浅源地震的分析 ,认为现今构造应力场和断裂对矿震等地质动力灾害的发生起控制作用 .一般说来 ,断裂的活动性及应力场性质不同 ,地质动力灾害发生的强度和频度也不同 .图 4,表 2 ,参 6 .     

海滩碎波带波性质的统计对比分析

利用台风影响下的海滩碎波带采集的两个测点的压力波资料从频域作了处理与计算 ,对波谱形态特征 ,有效波高、峰值周期、有效波陡、波的群性因子、碎波谱的平衡域和长重力波要素等相应的波性质作了对比分析。     

底层柱子不等长框架的地震反应研究

短柱几种不同长度情况，用ANSYS有限元程序进行了弹性地震反应的时程,总结了这种框架的地震反应规律。     

琼西戈枕剪切带金矿同位素地球化学

琼西戈枕剪切带控制的金矿床，产于前寒武系变质岩系中，区域上沿构造带呈北东向展布，从北东南南西有土外山－抱板金矿区，二甲金矿区和不磨金矿区等，构成了海南岛目前最有工业价值的金矿成矿带。对该成矿带典型矿床同位素地球化学的研究，表明其成矿物质主要来自抱板群混合岩系，但有部分深源物质的叠加；成矿流体主要是混合岩化热液和大气降水热液的混合，局部有岩浆热液参与，其深部物质和岩浆热液的叠加受剪切带变形环境和后期岩浆活动的控制；同位素组成在该区域有明显变化规律，并与构造变形，变质作用及其演化特点有关，这对剪切带与金矿成矿，成矿规律和成矿预测有重要意义。     

InSAR技术在西藏玛尼强震区的应用

为测量 1997年 11月 9日西藏玛尼里氏 7.4级地震震前一年的地壳形变和震时同震形变 ,以地震震中为图像中心的 5 0 km× 5 0 km范围内 ,选择了 5景 ERS- 1/ 2数据组成5个像对 ,并在此基础上组成 2个差分像对 ,以分别表示地震前一年形变和同震形变 ,再应用合成孔径雷达干涉测量(In SAR)技术进行处理。在同震形变差分图上 ,地震断层作用清晰可辨 ,在卫星斜距方向上可测量出近 0 .5 m的形变。结果表明 :In SAR技术对于定量研究同震形变和地震断层具有特别的优势和广阔的应用前景     

多点地震动时程人工合成

分析大跨度结构需要一种效率、精度都较高的多点地震动时程合成方法。基于平稳随机过程理论推导了多点地震动时程合成公式，每一频率点处的时程幅值与迟滞相干矩阵特征值和特征向量有关。用数值计算研究了迟滞相干矩阵特征对的变化规律，提出了对其进行简化的方法，用算例验证了简化计算的可行性。     

Apatite fission track dating evidence on the tectonization of Gangdese block, south Qinghai-Tibetan Plateau

This work makes the quantitative constrain on tectonizations of the Gangdese block, south Qinghai-Tibetan Plateau. Apatite fission track (AFT) dating analyses of 15 samples collected across the Gangdese block show that the Gangdese block went through two periods of tectonizations, during ~37.2 - 18.5 Ma and 18.5 - 8.0 Ma in the south Gangdese block, and during ~47.6 - 5.3 Ma and 5.3 - 0 Ma in the middle Gangdese block. Different upliftings did not take place in the first period and rapid uplifting occurred in the late period. Meantime, there are some differences between the south and middle Gangdese block. Their uplifting rate is 180 m/Ma and 70 m/Ma respectively. The rapid uplifting time in the middle Gangdese block lagged behind the time in the south Gangdese block. It is Chala-Jiacuo-Riduo fault zone that is similar to the Yarlung Zangbo fault zone in control of the tectonization.     

40Ar-39Ar ages of the Louzidian-Dachengzi ductile shear zone near Chifeng,Inner Mongolia and their tectonic significance

The Louzidian normal fault occurs as the eastern detachment fault of the Kalaqin metamorphic core complex. Field observations and microstructural analyses reveal that the Louzidian-Dachengzi ductile shear zone developed in its lower-plate was genetically related to sinistral strike-slips and extensional faulting. Two samples from this ductile shear zone yield 40Ar-39Ar plateau ages of 133 Ma (Bi) and 126 Ma (Kp), which are concordant with their isochron ages. The plateau age of 133 Ma (Bi) records the formation age of the ductile shear zone. The inconsistent relationship between the earlier strike-slip ductile shear zone and the later normal fault makes the Kalaqin Quasi-metamorphic core complex distinctive from Cordilleran metamorphic core complex. These ages provide important geochronological data for putting constraints on the formation age and genesis of such ductile shear zones.     

A Study of the Crustal Stability in the Yangtze Three Gorges Area

TheThree GorgesHydroelectricPow erProjectontheYangtzeRiverwillstorewaterandgenerateelectricpowerin 2 0 0 3.Itsgreatdamwasdesignedtobe 1 85mhigh ,withaninstallingcapa bilitytobe 1 7.6 8millionkWh ,andatotalreservoirstoragetobe 39 3billionm3 .ThisisanimportantmatterinChina seconomicconstructionandalsoamonumentalprojectinChinesehistory(Fig 1 ) [1 ] .Thus,thecrustalstabilityforthegreatdamhasattractedmuchat tention .Theauthorshadcarriedoutfieldinvestigationanddemonstratedthefeasibilityoftheeng…     

遗传算法的新改进--扰动式遗传算法

针对基于二进制编码遗传算法的精度低及二进制编码所带来的早熟等问题提出了一种新的改进方案--扰动式遗传算法(简称DGA),该方法通过对搜索区域进行微小的扰动而实现不同群体之间的竞争来提高算法的搜索性能.改进后的算法在提高精度的同时能够达到全局收敛,并能有效地处理多极值问题.对改进的算法进行了性能分析并用典型函数进行测试,结果表明,改进的效果较为显著.