铅芯橡胶支座隔震钢框架结构体系振动台模型试验研究

设计并完成了铅芯橡胶支座隔震钢框架结构体系的振动台模型试验,研究刚性地基上隔震结构体系的动力特性和隔震效果,为进一步开展考虑土-结构相互作用的隔震结构体系振动台模型试验提供数据对比。试验结果表明:刚性地基上隔震结构体系具有良好的隔震性能,隔震效果显著,输入地震动的频谱特性和加速度峰值对隔震结构的隔震效率影响较大。     

云南哀牢山金矿带大坪韧性剪切带型金矿40Ar-39Ar定年

云南大坪金矿是哀牢山金矿带中最重要的金矿之一,主要赋存在受到强烈韧性剪切和水-岩反应的加里东期闪长岩中,是典型的韧性剪切带控矿型金矿。本文对大坪金矿绢英岩化近矿围岩中的热液绢云母进行了40Ar-39Ar定年,得到其坪年龄为33.76±0.65Ma,相应的反等时线和正等时线年龄分别为33.55±0.74Ma和33.57±0.74Ma,显示大坪属于喜马拉雅早期金矿。这些年龄数据与哀牢山金矿带中广泛出现的喜马拉雅期煌斑岩脉年龄(33～34Ma)非常接近,显示金矿与上地幔部分熔融形成的煌斑岩之间可能存在成因上的联系。喜马拉雅早期,本区在地壳拉张和强烈韧性剪切条件下,Moho面上升,地幔物质部分熔融并上涌,形成大量煌斑岩等基性岩脉,地幔排气形成的深源地幔流体和下地壳脱水形成的富CO2流体混合,沿韧性剪切带上升,并与糜棱岩化的加里东期闪长岩围岩发生水-岩反应,局部发生流体沸腾作用,导致成矿流体物理化学条件的改变和矿石矿物的沉淀,在剪切带脆性构造中形成含金石英脉。     

变截面桩的力学性能及工程意义

通过对变截面桩的荷载传递性质及变形特性详细分析,指出其具有受力合理,沉降小等优点,并通过工程实例进行了验证。     

考虑上部结构的桩筏基础非线性共同作用分析

当前虽然已有考虑桩筏非线性的设计,但仍无人在此基础上,考虑上部结构。因此考虑上部结构,进一步认识其与桩筏基础非线性共同作用机理,优化桩筏基础设计,具有重要的现实意义。本文以子结构法凝聚上部结构的荷载及刚度,以平面壳体单元模拟筏板,按有限层法模拟桩土之间的弹性相互作用,用广义剪切位移法模拟桩的非线性工作性状,建立了一种考虑上部结构共同作用的桩筏基础非线性分析方法,并编制了分析程序。通过实例分析,探讨了上部结构与桩筏基础非线性共同作用的机理,研究了合理布桩方式,探讨了以差异沉降为目标的优化设计的可能途径。     

巧用CASIO fx-4800P计算器测设线路复合曲线

介绍应用地面点与线路中线相对关系的统一数学模型,使用CASIOfx-4800P程序型计算器编制适合野外测设线路各种复合曲线(包括直线、缓和曲线、圆曲线的任意组合)的实用程序。     

基于三维破坏面的地基极限承载力计算方法

为确定作用在给定基础形状地基土上的极限承载力,对基底下的土体进行网格划分,先假定一矩形均布荷载作用在此地基土上,运用布氏解的积分公式,结合角点法,编制MATLAB语言程序,求出每个网格结点上的附加应力,进而求得每个网格结点上的主应力,根据破坏准则,由程序找出破坏点的坐标,利用MATLAB的图形处理功能,把破坏点的坐标在坐标图中显示出来。继续加大矩形均布荷载,直至这些破坏点在坐标图中刚好能够形成一个连续的破坏面,此时的矩形均布荷载即为该地基的极限承载力。此方法不仅可以有效地避免地基承载力经验公式中一些不合理的假设带来的误差,更符合实际情况,而且可以直观地了解到地基土的三维破坏面。     

富峰山玄武岩时代火山事件的划分及地质找矿意义

依据地质及同位素测年资料,富峰山玄武岩的地质时代为晚白垩世.按火山事件地层学的观点,当前至少可划分出6次火山事件.这些火山活动在松嫩盆地地下所携带的幔源气体与一些重要气藏密切相关.火山活动的特点疏中生代而亲新生代,表明它是由中生代陆缘火山弧发展阶段向新生代盆岭发展阶段转折的重要时期.     

不同类型GPS基线向量构成的控制网平差探讨

从工作实践中遇到的问题着手，通过对不同GPS接收机施测的同一条边的基线向量存在的差异进行分析，探讨了应用Helmert方差分量估计公式求GPS基线向量的方差分量，阐述了应用TGPPS4．03版软件进行平差的方法。     

LATE QUATERNARY ACTIVITY OF FAULTS IN THE EPICENTER AREA OF JINGGU M6.6 EARTHQUAKE

The 2014 Jinggu M6.6 earthquake attacked the Jinggu area where few historical earthquakes had occurred and little study has been conducted on active tectonics. The lack of detailed field investigation on active faults and seismicity restricts the assessment of seismic risk of this area and leads to divergent view points with respect to the seismotectonics of this earthquake, so relevant research needs to be strengthened urgently. In particular, some studies suggest that this earthquake triggered the activity of the NE-trending faults which have not yet been studied. By the approaches of remote sensing image interpretation, structural geomorphology investigation and trench excavation, we studied the late Quaternary activity of the faults in the epicenter area, which are the eastern margin fault of Yongping Basin and the Yixiang-Zhaojiacun Fault, and drew the conclusions as follows: (1)The eastern margin fault of Yongping Basin originates around the Naguai village in the southeastern margin of Yongping Basin,extending northward across the Qiandong, Tianfang, and ending in the north of Tiantou. The fault is about 43km long, striking near SN. The linear characteristic of the fault is obvious in remote sensing images. Structural geomorphological phenomena, such as fault troughs, linear ridges and gully dislocations, have developed along the faults. There are several dextral-dislocated gullies near Naguai village, with displacements of 300m, 220m, 146m, 120m and 73m, respectively, indicating that the fault is a dextral strike-slip fault with long-term activity. In order to further study the activity of the fault, a trench was excavated in the fault trough, the Naguai trench. The trench reveals many faults, and the youngest strata offseted by the faults are Holocene, with ¹⁴C ages of(1 197±51)a and(1 900±35)a, respectively. All those suggest that it is a Holocene active fault. (2)The Yixiang-Zhaojiacun Fault starts at the southeast of the Jinggu Basin, passes through Xiangyan, Yixiang, Chahe, and terminates at the Zhaojiacun. The total length of the fault is about 60km, and is a large-scale NE-trending fault in the Wuliangshan fault zone. Four gullies are synchronously sinistrally dislocated at Yixiang village, with the displacements of 340m, 260m, 240m and 240m, indicating that the fault is a long-term active sinistral strike-slip fault. A trench was excavated in a fault trough in Yixiang village. The trench reveals a small sag pond and a fault. The fault offsets several strata with clear dislocation and linear characteristic. The thickness of strata between the two walls of fault does not match, and the gravels are oriented along fault plane. The offset strata have the ¹⁴C age of(2 296±56)a, (3 009±51)a, and(4 924±45)a, respectively, and another two strata have the OSL age of(1.8±0.1)ka, (8.6±0.5)ka respectively, by which we constrained the latest paleoearthquake between(1.8±0.1)ka(OSL-Y01)and(378±48)a BP(CY-07). This again provides further evidence that the fault is a Holocene fault with long-term activity. (3)Based on the distribution of aftershocks and the predecessor research results, the 2014 Jinggu M6.6 earthquake and the M5.8, M5.9 strong aftershocks are regarded as being caused by the eastern margin fault of Yongping Basin, which is part of the Wuliangshan fault zone. The seismogenic mechanism is that the stress has been locked, concentrated and accumulated to give rise to the quakes in the wedge-shaped area near the intersection of the SN and NE striking faults, which is similar to the seismogenic mechanism in the southwest of Yunnan Province.     

ANALYSIS OF TYPHOON MATSA （NO.0509） AFFECTING SHANDONG PROVINCE

The characteristics of the moving course of Typhoon Matsa (No.0509), associated heavy rain and physical quantities fields have been analyzed, with the focus on the reason of the typhoon’s abrupt northeastward turn in Anhui Province and heavy rain concentrating in the northeast of typhoon center instead of near it. Meaningful conclusions are as follows. The reasons for typhoon abrupt turning are that the subtropical high pressure was moving southward and divergence fields of 200 hPa were to the right of the typhoon center; there was no obvious cold air invading Shandong after the typhoon entered the westerly belt; the southeasterly jet of typhoon and shear brought heavy rainfall to the Shandong peninsula before the typhoon entered Shandong. But after the typhoon’s movement into Shandong, the typhoon’s inverted trough brought the rainfall to the northern and central Shandong.