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排序方式: 共有41条查询结果,搜索用时 15 毫秒
1.
In this paper, statistics are taken on the co-seismic response of underground fluid in Yunnan to the Nepal MS8.1 earthquake, and the co-seismic response characteristics of the water level and water temperature are analyzed and summarized with the digital data. The results show that the Nepal MS8.1 earthquake had greater impact on the Yunnan region, and the macro and micro dynamics of fluids showed significant co-seismic response. The earthquake recording capacity of water level and temperature measurement is significantly higher than that of water radon and water quality to this large earthquake; the maximum amplitude and duration of co-seismic response of water level and water temperature vary greatly in different wells. The changing forms are dominated by fluctuation and step rise in water level, and a rising or falling restoration in water temperature. From the records of the main shock and the maximum strong aftershock,we can see that the greater magnitude of earthquake, the higher ratio of the occurrence of co-seismic response, and in the same well, the larger the response amplitude, as well as the longer the duration. The amplitude and duration of co-seismic response recorded by different instruments in a same well are different.Water temperature co-seismic response almost occurred in wells with water level response, indicating that the well water level and water temperature are closely related in co-seismic response, and the well water temperature seismic response was caused mainly by well water level seismic response. 相似文献
2.
Haruko Sekiguchi Masayuki Yoshimi Haruo Horikawa Kunikazu Yoshida Sunao Kunimatsu Kenji Satake 《Journal of Seismology》2008,12(2):185-195
We studied the long-period ground motions in the Osaka sedimentary basin, Japan, which contains a 1- to 3-km thickness of
sediments and is the site of many buildings or construction structures with long-natural period. We simulated the broadband
ground motions likely to be produced by the hypothetical Nankai earthquake: the earthquake expected to give rise to the most
severe long-period ground motion within the basin. For the simulation, we constructed multiscale heterogeneous source models
based on the Central Disaster Management Council of Japan (CDMC) source model and adopted a hybrid computation method in which
long-period motion and short-period motion are computed using a 3-D finite difference method and the stochastic Green’s function
method, respectively. In computing long-period motions, we used a 3-D structure model of the crust and the Osaka sedimentary
basin. The ground motions are estimated to have peak velocities of 50–90 cm/s, prolonged durations exceeding 300 s, and long
predominant periods of 5–10 s in the area with great thickness of sediments. The predominant periods are in agreement with
an approximate evaluation by 4 H/V
s where H and V
s are the thickness of the sediment and the average S wave velocity, respectively. 相似文献
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本文对强震前震源系统的调制比r_m和调制比异常面积Sr_m随时间变化的起伏加剧现象进行回顾性研究,得到下列研究结果:(1)强震前近源区以及中强震前近源区大多出现调制比r_m的起伏加剧,并大多在起伏频次达三次时有大震或中强震发生。(2)大多数中、强地震前r_m异常面积Sr_m围绕震源区呈现由小至大、由大至小的过程,因此引入最小异常面积Sr_(min)和最大异常面积Sr_(max)之比γ作为中、短期预报指标,根据统计得到异常指标[γ]如下式某些震例在震前出现异常面积Sr_m起伏的加剧过程,初步认为是震源区周围调整单元调整能力较差导致的结果。(3)r_m、Sr_m起伏加剧开始时间与震级有关,震级愈大,起伏加剧出现愈早。根据半年步长逐月滑动得到的r_m-T图,起伏加剧开始至发震的时间与震级M的统计,得到如下关系(T以月计)M=4.29+0.11T(4)强震前场区异常一般呈现随机异常型、波动型和衰减型三种。若场区某统计区出现r_m的三次起伏加剧时,说明该统计区未来有强震发生。(5)由自治系统和非自治系统原理初步解释了震前震源区周围调整区调制比r_m及调制比异常面积Sr_m起伏现象的周期特征。 相似文献
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地震活动时序谱的涨落统计特征与地震活跃期 总被引:1,自引:0,他引:1
为寻求地震活动演化的统计判据,本文采用多项式拟合法展示地震时序谱之涨落谱,以分维函数法判断最小邻间距(NNS)分布的Poisson性,然后采用MKS无参量法判别涨落谱之统计稳定性,确定NNS分布的转变区,具体研讨了四川、云南若干震区地震活动时序谱的涨落统计分布,发现地震活跃期到来时NNS分布表现出非Poisson化的特征。进一步通过改变和调节时序数据样本集之震级下限,并逐段前推进行统计计算的方式进一步验证结果的可靠性,客观地确定了这些震区地震活动时序涨落谱统计特征的转变期,使根据该统计法判断地震活跃期的方法论渐趋完善。 相似文献
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中国热带第四纪气候波动幅度问题 总被引:2,自引:2,他引:2
根据40多个有关气候波动的实例分析,中国热带第四纪几个特征时段比今升温的幅度为1.0~3.0℃:降温幅度较大者为3.0~7.0℃,较小者为1.0—3.0℃。而中国热带地区现代理论雪线高度约为4300m;北半球长年冻土地带南界的年均温为-6.0~-8.0℃。因此,中国热带除台湾岛外,第四纪不具备形成冰川或冰缘现象的气候条件。 相似文献