天山内部博罗可努断裂精河—阿拉山口段晚更新世以来的活动特征   总被引：1，自引：0，他引：1       下载免费PDF全文

杨晓平  沈军 《地震地质》2000,(3)

通过对博罗可努断裂精河—阿拉山口段微地貌的实地调查 ,发现该断裂错断精河东南到阿拉山口之间的晚更新世冲洪积扇 ,地表留下了冲沟和山脊同步右旋位错、断层陡坎、断层鼓包、拉分盆地等与断层活动有关的微地貌。精河东南冲洪积扇上大冲沟的最大右旋位移为 50 0m ,平均4 0 0m。断层陡坎上的纹沟右旋位移为 2 6～ 4 0m ,较大级别的纹沟位移可分为 5 7m ,8 3m和 15 3m3组。它们大致为 3的整数倍。实测断层陡坎的高度分别为 1 2m ,2 51m和 3 6 3m ,大致是 1 2的整数倍 ,阿拉山口西南断层的水平位移为 1～ 1 7m ;垂直位移可分为两组 ,一组为 0 55m ,另一组为 1 2～ 1 5m。这些数据可能揭示了该断裂段的特征地震水平位移为 3m ,垂直位移为 1 2m。区域地貌对比和年代学分析得出 ,精河东南冲洪积扇的最后形成时代为距今 7万a左右 ,右旋滑动速率为4 7mm/a。  相似文献   

Activity Features and Slip Rate of the Lingwu Fault in Late Quaternary     

Liao Yuhu  Chai Chizhang  Zhang Wenxiao  Xu Wenjun 《中国地震研究》2000,14(4):329-337

The I ingwu fault is in the eastern boundary of the southern section of Yinchuan graben. It hasa close relation to seismicity in the Lingwu-Wuzhong region.Few researches have been done.In this Paper,on the basis of tee data obtained from field investigation,the activity features inLate Quaternary have been discussed.The vertical displacement and its slip rate have been alsoestimated.The fault is 48km in length,being divided into 3 segments according to geologicaland topographical characteristics.The last rupture along its northern and middle segments wasoccurred in late of Late Pleistocene or early Holocene while that along the southern segmentwas occurred in midle Holocene.The vertical slip rate is estimated as 0.23～025mm/a sinceabout 66ka B.P.based on the vertical displacements of terracesⅠ,Ⅱ and Ⅲ and their ages.  相似文献   

吐哈盆地杜家台构造侏罗系生油岩热演化特征     

卢延恩  纪友亮 《矿产与地质》2000,14(1):39-43

利用干酷根镜质体反射率等多项指标分析了吐哈盆地杜家台构造侏罗系生油岩的热演化特性,认为该构造上生油岩生油门际在３５６０ｍ左右。侏罗系七克台组、三间房组、三工河组的生油岩处于未成熟阶段,西山窑组和八道湾组也尚进入生油阶段。八道湾组煤系地层成熟度高,是入亮煤阶段,煤成气生成量多,是重点勘探层。  相似文献   

重组鱼类生长激素对中国对虾成活率及促生长作用的研究   总被引：2，自引：0，他引：2  

徐斌  张培军  麦康森  徐永立  苗宏志 《海洋科学》2000,24(11):54-56

１１９９９９３３年年后后暴暴发发性性对对虾虾病病毒毒病病的的流流行行 ,,严严重重制制约约着着对对虾虾养养殖殖的的进进一一步步发发展展。。如如何何通通过过促促进进中中国国对对虾虾生生长长 ,,提提高高其其抗抗病病力力已已成成为为目目前前亟亟待待解解决决的的问问题题 ;;其其中中通通过过在在对对虾虾人人工工饵饵料料中中加加入入一一些些生生长长因因子子 ( (如如生生长长激激素素等等 ))或或满满足足对对虾虾的的各各种种营营养养需需求求 ,,提提高高中中国国对对虾虾的的生生长长速速度度与与抗抗病病力力是是解解决决这这…  相似文献   

华北地区断层形变异常与地震活动   总被引：2，自引：0，他引：2  

郭良迁  薄万举  杜雪松  谢觉民  陈银河 《地震》2004,24(3):42-50

根据断层形变求解的华北地区异常参数和应变累积率, 研究了华北主要断裂带的断层形变异常及其应震特征。 同一断裂带上的形变异常与该带上的地震有较好的对应性。 河套—张家口—蓬莱活动构造带上发生的强震, 北京地区的断层形变异常参数在总体上几乎都有明显的前兆性异常。 山西带北部的断层形变异常参数对山西断陷带及其延伸部位上的强震同样有较好的反映。 断层应变累积率反映了应力的积累程度, 其值相对较大时, 测点所在地区的地震较活跃, 反之亦然。  相似文献   

兴仁县罗马山滑坡体形变监测及成因分析          下载免费PDF全文

章彭  刘文明 《贵州地质》2020,37(1):94-97

InSAR技术是当前从卫星雷达遥感获取的对地观测数据中提取地形信息最主要的技术手段。本文以贵州省普安县罗马山为研究区,收集了2017年4月16日至2018年8月5日共10景ALOS PALSAR2数据,生成9个干涉对,以形变时间序列的方式对研究区中的滑坡体进行形变监测分析。同时,收集兴仁县2017年4月至2018年8月降雨量信息,通过与形变时间序列的对比分析,可发现降雨量与形变的高度相关性,这对滑坡灾害的预防具有重要意义。  相似文献   

Estimation of Longshore Sediment Transport Rate for a Typical Pocket Beach Along West Coast of India     

V. Noujas  R. S Kankara  K. Rasheed 《Marine Geodesy》2018,41(2):201-216

Estimation of Longshore Sediment Transport Rate (LSTR) in the littoral zone is essential for managing and developing any coastal zone. Numerical models are powerful tool to understand and investigate various processes responsible for LSTR in a systematic manner since direct measurement of LSTR is a difficult task. A one dimensional LITDRIFT model was implemented along the Vengurla coast for estimation of LSTR and to analyze the sensitivity of each input parameters towards the computation of LSTR. Major input parameters required for the estimation of LSTR are nearshore wave climate, bathymetry, and sediment characteristics. The nearshore wave data at a depth of 15 m were collected using wave rider buoy in 2015 is used in the present study. Field observations were carried out to survey the regional bathymetry and sediment characteristics. Annual net LSTR along Vengurala coast is relatively less and varies from ?7778 to ?9015 m³ with an average of ?8511 m³. The net direction of LSTR is towards south and gross LSTR is 1.18 × 10⁵ m³/year. The LSTR reveals more sensitivity to coastline orientation and wave direction. A 1° changes in coastline angle and wave direction causes approximately 3000 m³/month difference in LSTR. Moreover, wave height, wave period, and bed roughness has an important role for controlling LSTR. The model results help to identify the role of each parameter contributing towards LSTR estimation and a similar model approach can be applied to other coasts for estimating LSTR in an accurate way.  相似文献   

2008年MS7.1于田地震InSAR同震形变场及其震源滑动反演   总被引：9，自引：1，他引：8       下载免费PDF全文

张国宏  屈春燕  单新建  张桂芳  宋小刚  汪荣江  李振洪  胡植庆 《地球物理学报》2011,54(11):2753-2760

本研究利用InSAR技术与ALOS PALSAR雷达数据,获取了2008年3月20日于田MS7.1地震视线向同震形变场,并基于该数据集和限制性最小二乘算法反演了此次地震的断层滑动分布;通过构造四大类反演方案,详细分析了InSAR观测系统中的入射角与方位角对反演结果的影响.结果表明:入射角随点位变化对反演结果有较大影响,...  相似文献   

2021年青海玛多M_W7.4地震GNSS同震形变场及其断层滑动分布     

王迪晋  王东振  赵斌  李瑜  赵利江  王阅兵  聂兆生  乔学军  王琪 《地球物理学报》2022,65(2):537-551

2021年5月22日青海玛多M_W7.4地震作为发生在巴颜喀拉块体内部的一次强震,再次引起了人们对该地区地震活动性的强烈关注.本文基于震后GNSS流动观测和区域连续GNSS站资料,解算了106个站点的同震形变及其中17个站点的高频形变波形.同震形变场显示玛多地震具有典型的左旋走滑特征,GNSS观测到的最大同震位移达到1.2 m.GNSS与InSAR数据相符度较高,GNSS提供了准确的近场形变信息.基于GNSS同震形变场,本文反演了断层滑动分布,并计算了发震断层上产生的库仑应力变化.结果表明,发震断层的滑动破裂存在多个凹凸体,破裂分段特征明显且出露地表,与野外地表破裂考察和余震分布吻合,主体破裂位于断层面0~10 km的浅部区域,最大滑动量达到4.6 m,地震矩1.63×10²⁰N·m,矩震级为M_W7.4;发震断层上静态库仑应力增加区域与余震分布具有一致性,说明余震主要是由静态库仑应力加载而触发的.  相似文献   

Sheath fold morphology in simple shear     

《Journal of Structural Geology》2013

Sheath folds are highly non-cylindrical structures often associated with shear zones. We investigate the formation of sheath folds around a weak inclusion acting as a slip surface in simple shear by means of an analytical model. We present results for different slip surface orientations and shapes. Cross-sections perpendicular to the shear direction through the sheath fold display closed contours, so called eye-structures. The aspect ratio of the outermost closed contour is strongly dependent on the initial slip surface configuration. The center of the eye-structure is subject to change in height with respect to the upper edge of the outermost closed contour for different cross-sections perpendicular to the shear direction. This results in a large variability in layer thickness across the sheath fold length, questioning the usefulness of eye-structures as shear sense indicators. The location of the center of the eye structure is largely invariant to the initial configurations of the slip surface as well as to strain. The values of the aspect ratios of the closed contours within the eye-pattern are dependent on the strain and the cross-section location. The ratio (R′) of the aspect ratios of the outermost closed contour (R_yz) and the innermost closed contour (R_y′z′) shows values above and below 1. R′ shows dependence on the slip surface shape and orientation but not on the number of involved contours. Using R′ measurements to deduce the bulk strain type may be erroneous.  相似文献