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1.
正莫斯科时间2月15日早上7时30分左右,北京时间2月15日中午12时30分左右,俄罗斯车里雅宾斯克州有天体坠落。根据俄紧急情况部的说法,坠落的是一颗陨石。经俄罗斯官方证实,这颗陨石超过十吨重,  相似文献   

2.
USGS中的汶川地震情况   总被引:1,自引:0,他引:1  
1地震参数震级:MW7.9。发震时间:2008年5月12日06时28分01秒(UTC)。当地时间5月12日14时28分01秒。震中位置:30.986°N,103.364°E。震源深度:19km。震中:中国四川省东部。震中位于:成都西北偏西80km,绵阳西南偏西150km,重庆西北偏西350km,北京西南1545km。定位不确定性:水平方  相似文献   

3.
正"车里雅宾斯克上空正在举行‘愤怒的小鸟'世界杯赛(当地上空残留的一道白色烟雾,与‘愤怒的小鸟'游戏中的场景相吻合)!"一位亲见车里雅宾斯克陨石坠落的当居民戏称。当地时间2013年2月15日12时30分,在俄罗斯西部的车里雅宾斯克、斯弗罗夫斯克、巴什科尔托斯坦共和国的秋明和奥伦堡附近地区的民众,目睹了一块陨石坠落在俄罗斯车里雅  相似文献   

4.
一、地震的基本情况 1984年5月21日23时38分上海市大多数居民从睡梦中被一阵剧烈震动所惊醒。这是由于在南黄海域发生的一系列地震中最初连续发生的两次地震引起的。上海市的地震烈度达到了五度。根据国家地震局地球物理研究所的中国台站临时报告提供的资料,1984年5月21日15时37分50秒(GMT)在北纬32.7°N、东径121.6°E发生了一次震级M_S=5.6的地震,时过1分08秒,即15时38分58.1秒,在同一震中附近,即北纬32.688°N、东径121.5O9°E又发生了一次震级为M_B=5.9、M_S=6.3的地震,震源深度18km。对于这两次地震,美国地震情报  相似文献   

5.
《华南地震》2007,27(3):99-99
发震时间月44555666日6244122941229时8423182212523分50305735242638秒34.137.717.76.654.830.451.912震中位置北纬23°19′24°31′24°08′23°55′22°36′24°31′24°56′21°46′东经117°23′117°24′106°35′114°30′107°46′118°54′117°37′111°47′地点福建东山海域福建南靖广西凌云广东新丰江广西扶绥福建晋江海域福建华安广东阳江3.73.333.13.43.443.62019855-219震级/ML震源深度/序号km12345678华南地区M_L≥3.0级地震目录(2007-04~2007-06)~~…  相似文献   

6.
王建燕 《地球》2011,(11):55-56
纳米比亚霍巴陨石重约60吨 霍巴陨石是坠落在地球上的最重陨石,其表面积超过6.5平方米,重量在60吨左右。据说,在坠落地球过程中,霍巴陨石的飞行速度因与地球大气层之间发生的摩擦大大降低,使其在落地之时得以保持完整并且大部分露出地表,而不是埋入地下。其异乎寻常的扁平外形说明,这颗陨石甚至能够像漂石一样在水面上跳跃前进。  相似文献   

7.
2004年7月14日9时33分33秒在山西省盂县南娄镇(φN38°02′,λE113°25′)发生ML3.4地震,震源深度7 km.这次地震震感强烈,有感范围较大,东起盂县清城村,西到盂县王子台村,北起盂县县城,南到寿阳县温家庄村.地震发生后,阳泉市地震局的单台测震仪记录到这次地震.震后对震区进行了实地考察.在大约235 km2的范围内,完成了23个村的调查,调查建筑物28栋.  相似文献   

8.
<正>2015年4月15日15时39分28.6秒(北京时间),内蒙古自治区阿拉善盟阿拉善左旗发生MS5.8地震,中国地震台网给出该地震的震中位置为39.8°N,106.3°E,震源深度为10 km。此次主震后,发生多次余震,根据中国地震台网记录,于当日15时44分33秒在内蒙古自治区阿拉善盟阿拉善左旗发生M4.0地震(39.8°N,106.3°E)、当日18时49分58秒在内蒙古自治区阿拉善盟阿拉善左旗发生M3.1地震(39.8°N,106.4°E),两次  相似文献   

9.
正人类所处的地球,只是太阳系中一颗普通的行星,陨石来袭本也是常有之事,然而这一次发生在俄罗斯的陨石事件,陨石来势突然,毫无防备,造成了大量的人员受伤和巨额财产损失,引起了全世界的高度关注,产生了广泛的社会影响。俄罗斯媒体早在16日就报道,俄罗斯的陨石坠落事件已造成10亿卢布  相似文献   

10.
本月新闻     
伊朗中北部发生强烈地震  2 0 0 4年5月2 8日1 2时38分4 6秒(国际时) ,伊朗中北部发生了强烈地震。据德黑兰大学地球物理学研究所测定,此次地震的震级为里氏5 5级,震中位于马赞达兰省恰卢斯市郊区的巴拉代镇。美国国家地震信息中心(NEIC)公布的结果为:震中位于51 582°E ,36 2 74°N ,震源深度为2 8 5km ,震级为MS6 4 ;中国国家数字地震台网的快报结果为:震中位于36 32°N ,51 0 0°E ,震源深度为55km ,震级为MS6 6 )。震中距伊朗首都德黑兰大约70km ,距马赞达兰省首府沙里约1 35km。从伊朗里海各省到中部和西北部的8个省都有…  相似文献   

11.
苏门答腊--蒙古(1935~1957)地震大迁移的回顾   总被引:1,自引:0,他引:1  
为了分析2004年12月26日苏门答腊Ms8.9大地震对大陆地震形势的影响,本文介绍了1935~1957年苏门答腊-蒙古地震大迁移事件,时间持续22年,长度4600km,迁移速度205km/a。迁移以1935年12月28日苏门答腊Ms7.7地震为起点,从印度-澳大利亚板块与欧亚板块南部边界俯冲事件开始,向北经安达曼海沟到达缅甸弧和喜马拉雅弧东端后,进入中国大陆,沿着中蒙大陆中轴地震带直抵蒙古。  相似文献   

12.
为了分析2004年12月26日印度尼西亚苏门答腊Ms8.9级大地震对中国大陆地震形势的影响,介绍了1935~1957年的苏门答腊—蒙古地震大迁移事件,此迁移事件持续22a,长度4600km,迁移速度205km/a。迁移由1935年12月28日苏门答腊Ms7.7地震为起点,由印度—澳大利亚板块与欧亚板块南部边界俯冲事件开始,向北经安达曼海沟到达缅甸弧和喜马拉雅弧东端后,进入中国大陆,沿着中蒙大陆中轴地震带直抵蒙古。  相似文献   

13.
The Asian monsoon-arid environment system began to develop during the Oligocene, but the exact position of the arid zone boundary is uncertain in the Oligocene. Fossil mammal assemblages can be used to assess the environment of an area. There were two sizes of mammals in the Nanpoping fauna from the Oligocene strata of the Lanzhou Basin: the small ones were grassland rodents such as Ctenodactylidae; the large ones were forest dwellers such as Paraceratherium and Paraentelodon. Of the 23 species of mammals identified in the Nanpoping fauna, ~40% were forest dwellers and the rest (~60%) were grassland taxa. The Nanpoping fauna was compared with the contemporaneous Dingdanggou fauna in the Danghe area to the north and Jiaozigou fauna in the Linxia area to the south. The Nanpoping fauna contains elements of both other faunas and thus represents a transitional assemblage between forest and grassland. So, it can be inferred that the southern boundary of the arid zone in China during the Oligocene was probably near the Lanzhou Basin.  相似文献   

14.
岫岩陨石撞击坑结构高精度地震探测研究   总被引:4,自引:0,他引:4       下载免费PDF全文
我国的岫岩陨石撞击坑位于辽东半岛北部低山丘陵地区,直径1.8 km,保存完好,已被多方面的证据证实为陨石撞击坑.陨石的撞击和此后的沉积作用在坑内形成了特殊的地球物理场,使坑内与坑外的介质在速度、密度等方面存在差异.本次通过采用反射和折射地震相结合的探测方法,利用陨石撞击所形成的岩石的地震波速度和波阻抗差异,获得了陨石坑...  相似文献   

15.
On Wednesday 11th May 2011 at 6:47 pm (local time) a magnitude 5.1 Mw earthquake occurred 6 km northeast of Lorca with a depth of around 5 km. As a consequence of the shallow depth and the small epicentral distance, important damage was produced in several masonry constructions and even led to the collapse of one of them. Pieces of the facades of several buildings fell down onto the sidewalk, being one of the reasons for the killing of a total of 9 people. The objective of this paper is to describe and analyze the failure patterns observed in reinforced concrete frame buildings with masonry infill walls ranging from 3 to 8 floors in height. Structural as well as non-structural masonry walls suffered important damage that led to redistributions of forces causing in some cases the failure of columns. The importance of the interaction between the structural frames and the infill panels is analyzed by means of non-linear Finite Element Models. The resulting load levels are compared with the member capacities and the changes of the mechanical properties during the seismic event are described and discussed. In the light of the results obtained the observed failure patterns are explained. Some comments are stated concerning the adequacy of the numerical models that are usually used during the design phase for the seismic analysis.  相似文献   

16.
乌鲁木齐遥测地震台网和新疆地震台网的地震定位与分析   总被引:1,自引:0,他引:1  
利用新疆地震台网和乌鲁木齐遥测地震台网在乌鲁木齐地区100km范围内1993年6月至1993年12月10日各自定位的地震资料,以新疆地震台网为参考基准,将乌鲁木齐遥测地震台网的资料与其进行了对比。对比发现遥测地震台网比新疆地震台网在地震数量上多32.9%,在定位精度上也相对要高一些。另外,根据地震定位的三种交切结果,分析了遥测台网地震定位现状。  相似文献   

17.
This paper reports the results of an examination of the thermoluminescence (TL) of 23 meteorites which were observed to fall, and 17 meteorite finds which have had their terrestrial age determined by the14C method. The terrestrial ages of the observed falls range from 1 to 205 years, whilst the14C terrestrial ages range from 1200 ± 2000 to >20,000 years. A statistically significant correlation has been observed between the natural TL — as expressed as the ratio of the intensity of the low-temperature TL peak to that of the high-temperature peak — and the terrestrial age of the 40 meteorites. Furthermore, peak height ratios in excess of 3.0 are only observed in falls which fell within the last 250 years, suggesting that finds with peak height ratios as large as this, such as Allan Hills A77003 and Plainview (1917), fell within the last few hundred years. The present results are consistent with evidence that meteorite TL decay is a non-first-order process. The implications of the results for estimates of the terrestrial ages of 8 meteorite finds, for which there are no14C data, are also discussed.  相似文献   

18.
根据山西数字地震台网的地震震源深度资料,对山西测震台网2001年1月至2011年12月期间,2 535个定位精度为Ⅰ、Ⅱ类且ML≥2.0地震,进行震源深度分布特征统计分析。采用网格滑动平均法,统计平均震源深度,结果显示,山西地区平均震源深度为0~40km,从0~10km、11~20km、21~30km、31~40km不同震源深度分布结果来看,山西地区中小地震震源深度以6~20km为主,个别区域有大于20km的地震分布。  相似文献   

19.
收集了大三江盆地及其邻区区域地震台网及多个流动台阵的连续波形及远震事件资料,采用背景噪声层析成像和接收函数叠加方法,分别获得了研究区三维S波速度结构、基底及莫霍面深度和泊松比.结果显示:浅层速度结构较好地反映了地表地形及地质特征,三江盆地呈明显的低速,虎林和勃利等小型盆地的S波速度也相对较低,而小兴安岭、张广才岭等则呈...  相似文献   

20.
The Andaman-Sumatra Tsunami of Dec. 26, 2004, was by far the largest tsunami catastrophe in human history. An earthquake of 9 to 9.3 on the Richter scale, the extension of waves over more than 5000 km of ocean and run-ups up to 35 m are its key features. These characteristics suggest significant changes in coastal morphology and high sediment transport rates. A field survey along the west coast of Thailand (Phuket Island, Khao Lak region including some Similan Islands, Nang Pha mangrove areas and Phi Phi Don Islands) seven to nine weeks after the tsunami, however, discovered only small changes in coastal morphology and a limited amount of dislocated sediments, restricted to the lower meters of the tsunami waves. This is in striking contrast to many paleo-tsunami's events of the Atlantic region. Explanations for this discrepancy are sought in: a. Mechanics of the earthquake. A rather slow shock impulse on the water masses over the very long earthquake zone, b. Shallow water in the earthquake zone, and c. Bathymetry of the foreshore zone at the impacted sites. Shallow water west of Thailand has diminished wave energy significantly. The differences in geomorphological and sedimentological signatures of this tsunami compared with many paleo-tsunami worldwide makes it unsuitable to be used as a model for old and future tsunami imprints by an event of this extreme energy and extension.  相似文献   

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