柯坪断裂东段现今微动态运动监测与研究     

荆燕  张世中  熊玉珍  李宏  刘凤秋  孙起伟  董建业  张鸿旭  王海忠  陈葛天 《高校地质学报》2007,13(1):89-95

1997年1月2日~1998年12月31日新疆伽师地震群的发生,使柯坪断裂的滑动速率和运动方向发生了改变。利用MD系列断层仪对柯坪断裂东段的运动特征进行了观测与研究。结果表明,柯坪断裂带东段在伽师地震群前后,垂直滑动速率由0.037 mm/a提高到0.069 mm/a,水平错动速度由左旋0.033 mm/a改变为右旋0.016 mm/a;水平运动方向发生了改变,垂直运动强度提高了近一倍;伽师震群发生前后,柯坪断裂东段附近的应力场发生了改变,最大和最小水平应变率的大小虽未变化,但主应变率轴绕顺时针方向旋转了16.7°。  相似文献   

云南中甸-大具断裂马家村-大具段古地震初步研究     

程理  李光涛  吴昊  余建强  苏刚 《中国地震》2020,36(2):211-220

中甸-大具断裂马家村-大具段位于哈巴雪山北麓及玉龙雪山以北的大具盆地内,总体走向310°～320°,根据卫星影像解译和详细的野外地质地貌调查,认为中甸-大具断裂马家村-大具段自第四纪以来长期活动,横跨断裂的水系右旋位错量可分为8.5～12m、22m左右、47m左右、200～280m、500～510m和1000m左右6个等级。在大具盆地内发现了长约600m的地震地表破裂带,这是该断层段在全新世活动的直接地质证据,在破裂带南东端附近开挖的探槽揭示出自晚更新世以来断裂存在三期活动,可能对应3次地震事件,结合前人在该断裂段获得的地质剖面和断错地貌面测年结果,分析认为马家村-大具段自晚更新世以来至少发生了3次古地震事件,发生时间分别为4910～45 a BP、7000 a BP左右和32.93～19.96ka BP,利用垂直同震位移值估算了水平同震位移量,最终得出每次地震事件的震级为7.5级左右。  相似文献   

SLIP RATES OF THE RIYUE MT. FAULT AT DEZHOU SEGMENT SINCE LATE PLEISTOCENE          下载免费PDF全文

LI Zhi-min  SU Peng  HUANG Shuai-tang  TIAN Qin-jian  YIN Xiang 《地震地质》2018,40(3):656-671

The Riyue Mt. Fault is a secondary fault controlled by the major regional boundary faults (East Kunlun Fault and Qilian-Haiyuan Fault). It lies in the interior of Qaidam-Qilianshan block and between the major regional boundary faults. The Riyue Mt. fault zone locates in the special tectonic setting which can provide some evidences for recent activity of outward extension of NE Tibetan plateau, so it is of significance to determine the activity of Riyue Mt. Fault since late Pleistocene to Holocene. In this paper, we have obtained some findings along the Dezhou segment of Riyue Mt. Fault by interpreting the piedmont alluvial fans, measuring fault scarps, and excavating trenches across the fault scarp. The findings are as follows:(1) Since the late Pleistocene, there are an alluvial fan f_p and three river terraces T₁-T₃ formed on the Dezhou segment. The abandonment age of f_p is approximately (21.2±0.6) ka, and that of the river terrace T₂ is (12.4±0.11) ka. (2) Since the late Pleistocene, the dextral strike-slip rate of the Riyue Mt. Fault is (2.41±0.25) mm/a. In the Holocene, the dextral strike-slip rate of the fault is (2.18±0.40) mm/a, and its vertical displacement rate is (0.24±0.16) mm/a. This result indicates that the dextral strike-slip rate of the Riyue Mt. Fault has not changed since the late Pleistocene. It is believed that, as one of the dextral strikeslip faults, sandwiched between the the regional big left-lateral strike-slip faults, the Riyue Mt. Fault didn't cut the boundary zone of the large block. What's more, the dextral strike-slip faults play an important role in the coordination of deformation between the sub-blocks during the long term growth and expansion of the northeast Tibetan plateau.  相似文献   

VARIATIONS OF THE GRAVITY FIELD AND QUANTITATIVE PARAMETER ANALYSIS BEFORE THE 2016 MENYUAN M_S6.4 EARTHQUAKE          下载免费PDF全文

WANG Tong-qing  CHEN Shi  LIANG Wei-feng  LIU Jin-zhao 《地震地质》2018,40(2):349-360

  相似文献   

VELOCITY STRUCTURE TOMOGRAPHY OF REGIONS DOWNSTREAM THE JINSHA RIVER BASED ON DENSE OBSERVATION          下载免费PDF全文

ZHANG Na  ZHAO Cui-ping  LI Chun-hong  ZHOU Lian-qing 《地震地质》2019,41(6):1380-1394

In this paper, the double difference seismic tomography method is applied to the phase arrival times of 7 465 seismic events to determine the hypocenter parameters of events as well as detailed 3D velocity structure at the northern segment of Xiaojiang Fault and its surrounding area. The data was recorded by 42 stations of the Jinshajiang River network from August 2013 to November 2016. At 2~6km, V_P and V_S present low velocity anomalies along the northern segment of Xiaojiang Fault, and the V_S anomaly is especially remarkable. On both sides of the Xiaojiang Fault, there also exist obvious P and S wave low velocity areas. These low velocity areas correspond to the terrain, lithology distribution and the watershed of Jinsha River at shallower layer in the study area. Starting from 6km, a NE-directed high V_P band along Zhaotong-Ludian and Huize-Yiliang Fault is formed on the eastern side of the northern segment of Xiaojiang Fault. V_S also shows the high value in the area bounded by Lianfeng Fault, Baogunao-Xiaohe Fault and Huize-Yiliang Fault. Above 10km depth, to the west side of the Xiaojiang Fault including the Ninghui Fault, V_P shows a significant low-velocity anomaly, while to the east side it presents high velocity feature. The Xiaojiang fault zone shows a significant low V_P from north to south in the study region, and the low velocity anomaly in the northern segment is relatively significant, especially the low velocity anomaly area reaches 15km deep around Qiaojia area. Beneath the Baihetan Dam, a significant low V_P area reaching to 5km deep is found. The earthquakes around the dam formed a strip from shallow to deep on the low-velocity area side. Whereas, a stable high-velocity area is found under the Wudongde Dam. The events relocation result shows that:all the focal depths in the study area are shallower than 20km, and the predominant focal depth is within 15km. Different from the NE-trending of the major faults in the study area, the relocated seismic events are obviously distributed nearly east-west along Matang Fault and Daduo Fault and the region around Huize. The focal depths of M_S6.5 Ludian earthquake sequences are shallower than 15km, and mostly less than 10km. The aftershocks within 2a after the Ludian M6.5 earthquake form two predominant bands of about 40km and 20km along near EW and SN direction, respectively.  相似文献   

龙门山断裂带南段岩石圈磁场变化分析   总被引：4，自引：3，他引：1       下载免费PDF全文

宋成科  倪喆  陈斌  袁洁浩 《地震工程学报》2019,41(6):1529-1535

根据巴颜喀拉块体东部2011—2014年3期岩石圈磁场年变化情况,结合地壳应力资料,重点分析龙门山断裂带南段的岩石圈磁场变化与应力积累的关系。该区域2011—2012年和2012—2013年岩石圈磁场变化明显弱于周边区域,实测地壳应力结果反映汶川M_S8.0地震震后应力积累水平很高。压磁效应分析认为汶川M_S8.0地震后该区域高应力积累、低应变率的动力学背景是控制该区域岩石圈磁场弱变化的主要因素。此外,芦山M_S7.0地震及康定M_S6.3地震前震中区存在局部岩石圈磁场水平矢量的弱变化现象,尤其是2012—2013年水平矢量大小和方向均与周边区域相比存在明显差异,这可能是两次地震的前兆异常。  相似文献   

郯庐断裂带鲁苏皖段及邻区地壳速度结构   总被引：9，自引：6，他引：9       下载免费PDF全文

黄耘  李清河  张元生  孙业君  毕雪梅  金淑梅  王俊 《地球物理学报》2011,54(10):2549-2559

郯庐断裂带是我国东部规模最大的深断裂带.为了揭示该断裂带的深部结构,本文利用江苏、安徽、山东、上海和浙江地震台网记录的近震到时资料,对8700个地震事件重新精确定位,进而开展了多震相地震走时成像法反演地壳速度结构.通过分析郯庐断裂带鲁苏皖段及邻区三维地壳速度结构图像,发现(1)研究区内不同构造块体具有差异明显的地壳速度...  相似文献   

重力异常反映的郯庐带中南段构造边界与应力场     

朱益民  余腾  王鑫  张鹏 《大地测量与地球动力学》2023,43(1):71-81

为解决传统基于重力场数据一阶导数定义的总水平导数和解析信号振幅存在无法均衡深浅异常振幅的问题,应用重力全张量梯度数据,提出改进的倾斜导数地质体边界识别方法NTD_M。经模型验证,NTD_M在收敛性、抑噪性和边界识别精度方面均有提升。利用NTD_M将郯庐带中南段及邻区划分为14个边界较为清晰的构造单元,借助垂线偏差数据对郯庐带中南段的构造应力场和壳幔密度差进行反演。结果显示,二者在水平方向上存在显著差异,在空间上显著相关,构造应力最大差异值约为16 MPa,壳幔密度差约为0.2 g/cm³,构造应力等值线密集处与构造单元划分的边界以及地震分布情况对应较好。郯庐带中段最大主应力方向为NEE-EW,南段主应力方向以EW-NWW为主,总体呈EW向,与震源机制解、地应力测量和GPS反演结果具有较好的一致性。  相似文献   

A NEW DISCOVERY OF ACTIVITY OF FUSHAN SECTION OF THE TAN-LU FAULT ZONE IN THE LATE QUATERNARY          下载免费PDF全文

ZHAO Peng  YAO Da-quan  YANG Yuan-yuan  ZHENG Hai-gang  WANG Xing-zhou  XU Hong-tai  FANG Zhen 《地震地质》2017,39(5):889-903

The east branch fault of Tan-Lu fault zone extends from Fengshan Town of Sihong County on the north shore of the Huaihe River in Jiangsu Province, into Fushan Town of Mingguang City on the south shore of Huaihe River in Anhui Province. The landform changes from Subei plain on the north of Huaihe River to Zhangbaling uplift area on the south of Huaihe River. The terrain rises gradually with larger relief amplitude. The Fushan section of the Tan-Lu fault zone is located in Ziyang to Fushan area of Mingguang City. The fault is shown in the satellite image as a clear linear image, and the fault extends along the east side of a NNE-trending hillock. In this section the Quaternary strata are unevenly distributed, which causes some difficulties in the study of recent fault activity.In recent years, the author has found that the fault of the Fushan section of the Tan-Lu fault zone on the south of the Huaihe River still has a certain control effect on the landform and the Quaternary strata. Based on satellite imagery and geological data, we select the appropriate location in the Fushan section to excavate the Santang trench Tc1 and Fushannan trench Tc2, and clean up the Fushannan profile Pm, which reveals rich phenomena of recent fault activity. Santang trench reveals three faults, and the faulting phenomenon is obvious. One of the faults shows the characteristic of right-lateral strike-slip normal faulting; Fushannan profile reveals one fault, with the same faulting behavior of right-lateral strike-slip normal fault. Comprehensive stratigraphic sample dating results indicate that the fault dislocated the middle Pleistocene strata, late Quaternary strata and early Holocene strata. All our work shows that the fault of Fushan section has intensive activity since late Pleistocene, and the latest active age can reach early Holocene. The latest earthquake occurred at(10.6±0.8)~(7.6±0.5)ka BP. The faults exposed by trenches and profiles show the characteristics of right-lateral strike-slip normal faulting, which reflects the complexity of the tectonic stress field in the area where the fault locates.  相似文献   

结合PCA、多尺度分割及SVM的ASTER遥感蚀变信息提取     

唐淑兰  曹建农  王凯 《遥感学报》2021,25(2):653-664

为了利用遥感影像进行更加精确的找矿预测,本文选择新疆东天山尾亚地区ASTER数据进行矿化蚀变信息提取方法研究。为了提高信息提取精度,本文提出了结合主成分分析(PCA)、多尺度分割和支持向量机(SVM)的遥感矿化蚀变信息提取方法。首先,分析ASTER数据的特征,选取各矿化蚀变信息的特征波段,对组合波段进行主成分分析,获得主分量图像;然后,对各主分量图像进行多尺度分割,并获得分割之后的均值图像;接着,提取训练样本,利用SVM对训练样本进行训练,采用试验方法求得最优核参数和松弛变量,构造最优SVM模型;最后,运用最优SVM模型完成矿化蚀变信息的提取。进行主成分分析时,铁染蚀变信息选择Band1、2、3、4组合,Al-OH基团蚀变信息选择Band 1、4、6、7组合,OH和CO32-基团蚀变信息采用Band 1、2、8、9组合。在运行SVM时采用了序列最小优化算法(SMO)进行求解,速度提高了12%。实验结果表明,与波段比值法、主成分分析法及基于光谱角和SVM的方法等3种方法相比,本文方法提取铁染蚀变信息、Al-OH基团蚀变信息及OH和CO32-基团蚀变信息的总体精度可达到87.98%、 90.01%及88.93%,Kappa系数分别为0.8011、0.8134及0.8023,与成矿区带、已知矿点和已有不同地质背景成矿特征相关性较好。  相似文献