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221.
222.
用改进的数学公式,便于用单钻孔资料和岩层复平求面理倾斜、求岩层厚度、求地层断距等多个课题。 相似文献
223.
丁建伟 《武汉大学学报(信息科学版)》1991,(3)
本文介绍用栅格数据进行图形叠置分析的方法,提出矢量数据转换为栅格数据的链拓扑法、减少栅格数据存储量的编码方法、根据模糊综合评判原理建立多因素综合评价数学模型以及叠置评价结果的类型格网合并的边界跟踪算法,最后给出一个实例说明栅格图形数据叠置分析方法在城镇规划中的应用。 相似文献
224.
Closed form analytic expressions for displacement and stresses at any point of either of the two homogeneous, isotropic, perfectly
elastic half-spaces in welded contact due to very long strike-slip dislocations are obtained. Both cases of vertical and horizontal
strike-slip dislocations are discussed in detail. Variation of the displacement with horizontal distance from the fault and
with vertical distance from the interface for a vertical strike-slip fault is studied numerically. 相似文献
225.
水平分量磁变仪标度值随记录n变化率的测定及应用 总被引:1,自引:0,他引:1
水平分量磁变仪标度值S随记录n的变化呈稳定的线性关系,但变化率Kn各地磁台仪器并不相同。用本文方法测定Kn可以获得满意的结果。Kn的精确测定可使水平分量磁变仪非线性记录的计算方法进入实用化,可以校正K尺或电磁转换函计算值使之更精确,从而提高地磁资料质量。 相似文献
226.
硬玉位错滑移系及流变学特征的研究 总被引:1,自引:0,他引:1
本文所研究的硬玉采自Sesia-Lanzo带(阿尔卑斯意大利段)。该带经历了高压低温榴辉岩相变质,其变质温压为550℃~600℃,1.5~1.6GPa。应用透射电子镜精细研究硬玉单晶的位错特征尚属首次,研究结果表明经天然变形的硬玉单晶中,发育有大量自由位错、位错壁、亚晶粒。自由位错密度大约为1×108/cm2,以刃型位错为主,也发育有少量螺位错。刃位错的伯氏矢量b为[001]和[110](b=7.16A;1/2(a+b)=6.6A)。 相似文献
227.
Fault dimensions,displacements and growth 总被引:15,自引:0,他引:15
Juan Watterson 《Pure and Applied Geophysics》1986,124(1-2):365-373
Maximum total displacement (D) is plotted against fault or thrust width(W) for 65 faults, thrusts, and groups of faults from a variety of geological environments. Displacements range from 0.4 m to 40 km and widths from 150 m to 630 km, and there is a near linear relationship betweenD andW
2. The required compatibility strains (e
s) in rocks adjacent to these faults increases linearly withW and with
and ranges frome
s=2×10–4 toe
s=3×10–1. These are permanent ductile strains, which compare with values ofe
s=2×10–5 for the elastic strains imposed during single slip earthquake events, which are characterised by a linear relationship between slip (u) andW.The data are consisten with a simple growth model for faults and thrusts, in which the slip in successive events increases by increments of constant size, and which predicts a relationship between displacement and width of the formD=cW
2. Incorporation of constant ductile strain rate into the model shows that the repreat time for slip events remains constant throughout the life of a fault, while the displacement rate increases with time. An internally consistent model withe
s=2×10–5, giving repeat times of 160 years and instantaneous displacement rates of 0.02 cm/yr, 0.2 cm/yr, and 2.0 cm/yr when total displacement is 1 m, 100 m, and 10 km, and slip increasing by 0.5 mm with each event, gives a good approximation of the data. The model is also applicable to stable sliding, the slip rate varying with ductile strain rate and withW
2. 相似文献
228.
Field survey of the 1994 Mindoro Island,Philippines tsunami 总被引:2,自引:0,他引:2
Fumihiko Imamura Costas E. Synolakis Edison Gica Vasily Titov Eddie Listanco Ho Jun Lee 《Pure and Applied Geophysics》1995,144(3-4):875-890
This is a report of the field survey of the November 15, 1994 Mindoro Island, Philippines, tsunami generated by an earthquake (M=7.0) with a strike-slip motion. We will report runup heights from 54 locations on Luzon, Mindoro and other smaller islands in the Cape Verde passage between Mindoro and Luzon. Most of the damage was concentrated along the northern coast of Mindoro. Runup height distribution ranged 3–4 m at the most severely damaged areas and 2–4 in neighboring areas. The tsunami-affected area was limited to within 10 km of the epicenter. The largest recorded runup value of 7.3 m was measured on the southwestern coast of Baco Island while a runup of 6.1 m was detected on its northern coastline. The earthquake and tsunami killed 62 people, injured 248 and destroyed 800 houses. As observed in other recent tsunami disasters, most of the casualties were children. Nearly all eyewitnesses interviewed described the first wave as a leading-depression wave. Eyewitnesses reported that the main direction of tsunami propagation was SW in Subaang Bay, SE in Wawa and Calapan, NE on Baco Island and N on Verde Island, suggesting that the tsunami source area was in the southern Pass of Verde Island and that the wave propagated rapidly in all directions. The fault plane extended offshore to the N of Mindoro Island, with its rupture originating S of Verde Island and propagating almost directly south to the inland of Mindoro, thereby accounting for the relatively limited damage area observed on the N of Mindoro. 相似文献
229.
粘滑失稳及其物理场时空分布的实验研究 总被引:6,自引:3,他引:6
摩擦滑动的物理场实验研究表明:(1)能量空间分布的差异是失稳的重要条件,单发型大事件常发生于高能量向低能量的突变带或高能量背景区内的相对低能量区;(2)单发型大事件的孕育过程常常经历若干个能量输入输出循环,产生多个前兆阶段,并在失稳前源区常有一个弱化过程。小震或群发型事件失稳前常常只有一个能量积累与强化的过程,失稳前兆阶段性反映较差;(3)粘滑失稳时断层的位错与声发射的大小未见明显关系 相似文献
230.
北京西山水平分层剪切流变构造初探 总被引:7,自引:2,他引:7
对比国内外关于变质岩区构造变形序列的实例,可知第一世代的构造变形几乎都以发育不同尺度的强烈扁平化平卧褶皱和有关的轴面流劈理或片理,以及近水平的韧性剪切带等构造组合为特征。北京西山的情况也不例外。这可能代表变质岩区早期构造变形的一种普遍模式,可能是地壳较深构造层次发生大规模透入性水平剪切流变的反映 相似文献