A multi-scale 3-D crust velocity model in the Hefei-Chao Lake area around the southern segment of Tanlu Fault Zone          下载免费PDF全文

Lingli Li  Huajian Yao  Song Luo  Junhui Li  Xiaoli Wang  Hongyu Ni  Ziwen Bao 《地震科学（英文版）》2021,34(4):344-357

Regional high-precision velocity models of the crust are an important foundation for examining seismic activity, seismogenic environments, and disaster distribution characteristics. The Hefei-Chao Lake area contains the main geological units of Hefei Basin, with thick sediments and the Chao Lake depression. Several major concealed faults of the southern NNE-trending Tanlu Fault Zone cross this area. To further explore the underground distribution characteristics of the faults and their tectonic evolutionary relationship with adjacent tectonic units, this study used ambient noise data recorded by a seismic array deployed in Hefei City and Chao Lake, constructing a 3-D velocity model at the depth of 1–8 km. Then a multi-scale high-resolution 3-D velocity model of this area was constructed by this new upper crustal velocity model with the previous middle and lower crustal model. The new model reveals that a high-velocity belt is highly consistent with the strike of the Tanlu Fault Zone, and a low-velocity sedimentary characteristic is consistent with the Hefei Basin and Chao Lake depression. The distribution morphology of high and low velocity bodies shows that the sedimentary pattern of Hefei-Chao Lake area is closely related to the tectonic evolution of the Tanlu Fault Zone since the Mesozoic. This study also identifies multiple low-velocity anomalies in the southeastern Hefei City. We speculate that strong ground motion during the 2009 Feidong earthquake (magnitude of 3.5) was related to amplification by the thick sediments in the Hefei Basin. We also discuss further applications of multi-scale high-resolution models of the shallow layer to strong ground motion simulations in cities and for earthquake disaster assessments.  相似文献   

螺旋藻多糖对给予环磷酰胺BALB/C小鼠的保护作用研究   总被引：7，自引：1，他引：7  

王友顺  黎露刚  吴侃  谢宗华  唐庆  倪金星  汪庭  方光如 《海洋科学》1997,21(6):36-39

研究了螺旋藻多糖（ＰＳ）对环磷酰胺（ＣＹ）引起的ＢＡＬＢ／Ｃ小鼠造血功能等损伤的保护作用。当给小鼠ＣＹ时能同时给予ＰＳ时，就能大大减轻因给予ＣＹ经起的造血功能障碍；能明显减缓动物因使用ＣＹ的致的体重下降以及能明显减低因ＣＹ作用的死亡率，提示使用ＰＳ对预防或减轻化疗制剂的危害是具有明显作用的。为临床化疗、放疗病人使用ＰＳ提供了依据。  相似文献   

厦门同安西柯对虾养殖池的细菌数量动态   总被引：10，自引：0，他引：10  

林美兰  倪纯治  刘文华  叶德赞  周宗澄  林燕顺  曾活水 《台湾海峡》1998,(2)

本文研究了对虾养成期间养殖池生态系中细菌的数量动态,探讨其变化规律与虾病的关系。结果表明,总细菌、弧菌和发光细菌在水体、底质和虾体中的数量变化各异。在水体各菌数与其环境因子的关系中,除了总菌数与COD存在着正相关外,其它的不存在相关性。虾体的总细菌、弧菌和发光细菌的数量（以细胞计）可以用来预报虾病,三者的阅值分别为107个　／g（湿重）、105个／g（湿重）和104介／g（湿重）。通过对对虾的细菌学跟踪监测,可以及时采取有效的应急防治措施。  相似文献   

海洋来源羽毛降解菌株的筛选、鉴定及酶学性质研究          下载免费PDF全文

张红岩  何瑾  杨梦莹  张妮  王芳  申乃坤 《应用海洋学学报》2022,41(2):338-346

微生物降解羽毛既可保护环境又能实现废物的资源化利用,具有显著的经济效益和社会效益。本研究从广西钦州港海鸭养殖淤泥筛选获得一株可高效降解羽毛的菌株Gxun-20,通过对该菌株形态特征、生理生化特性和16S rRNA基因序列进行分析,以确定菌株的分类,并对菌株产角蛋白酶的条件及酶学性质进行研究。结果表明：该菌为副短短芽孢杆菌(Brevibacillus parabrevis);菌株最适产酶条件为：温度34 ℃,初始pH 6.5,羽毛含量1.5%(质量分数),发酵48 h,角蛋白酶活性可达277.45 U/mL。菌株Gxun-20所分泌的角蛋白酶最适温度为50 ℃,且热稳定性较好,最适pH为7.5;金属离子Fe³⁺、Cu²⁺、Co²⁺、Fe²⁺和Mn²⁺对酶活性有显著抑制作用,而Ca²⁺、Na⁺对酶活性有明显促进作用;金属螯合剂乙二胺四乙酸(ethylene diamine tetraacetic acid, EDTA)可显著抑制酶的活性,蛋白酶抑制剂苯甲基磺酰氟(pheny methyl sulfonyl fluoride, PMSF)可完全抑制酶活性,表明该蛋白酶的活性中心含有金属离子和丝氨酸;异丙醇可使酶活性提高至129.34%,酶活性在十二烷基硫酸钠(sodium dodecyl sulfate, SDS)、吐温40溶液中保持稳定;酶的底物特异性结果表明,该酶对羽毛类β-角蛋白及酪蛋白降解能力较好,而对牛血清蛋白、I型胶原及人发类α 角蛋白降解能力较弱。海洋来源的副短短芽孢杆菌Gxun-20及其所产角蛋白酶在废弃羽毛降解方面具有良好的应用价值。  相似文献   

基于闭合环的InSAR解缠误差探测方法研究     

王霞迎  赵超英  刘媛媛  谷守周 《大地测量与地球动力学》2018,38(3):321-325

基于Sentinel-1数据,提出一种基于多个干涉图闭合环的残差探测解缠误差方法。以形变量较大的墨西哥城区为实验场,分别采用不同的闭合环对同一个干涉对进行探测,结果具有较好的符合性。  相似文献   

InSAR滑坡探测技术研究——以金沙江乌东德水电站段为例     

康亚  赵超英  张勤  刘晓杰 《大地测量与地球动力学》2018,38(10):1053-1057

采用3类InSAR产品和DEM数据开展金沙江流域乌东德水电站段的潜在滑坡探测,成功识别出多处已知和未知的滑坡点,并探测出滑坡体的形态及稳定性,提供了一种高效的大范围滑坡探测技术。同时采用小基线集InSAR技术对金坪子滑坡进行监测,不仅获得该滑坡的空间分区特征,也获取重点滑坡区的时间序列结果,并且与地面监测结果比较,精度达1.8 cm。展示了不同InSAR技术在不同尺度滑坡调查与监测中的应用特点。  相似文献   

层式滤波隔震垫     

娄霓  靳树才 《高原地震》2007,19(4):55-60

根据震相图展示的地震波运动规律,利用滚动摩擦阻力只相当滑动摩擦阻力1／40～1／60的力学效应,将轴承钢球呈层状重叠组合成隔震垫,可获得重复滤波效果,能高效降低地震对房屋建筑的作用力,达到提高地震安全度,降低建筑成本、节约建筑资源的目的。  相似文献   

活性炭柱分离－亚硫酸钠解吸萃取比色法测定痕量金     

刘汉初  倪桃英 《铀矿地质》1988,(2)

本文叙述了用活性炭色层柱分离、亚硫酸钠解吸、TMK-异戊醇萃取比色测定痕量金的方法。采用了以硫酸钴、铬酸钾和硫酸铜等无机盐配制模拟标准系列,可以长期使用。本法操作简单,快速,成本低,工效高。一人一天可以分析30个以上试样,能测定出1×10~(-3)ppm的金含量,适用于地质普查金矿中大批试样的分析。  相似文献   

Active tectonics of the Himalaya     

James F Ni 《Journal of Earth System Science》1989,98(1):71-89

The Himalayan mountains are a product of the collision between India and Eurasia which began in the Eocene. In the early stage of continental collision the development of a suture zone between two colliding plates took place. The continued convergence is accommodated along the suture zone and in the back-arc region. Further convergence results in intracrustal megathrust within the leading edge of the advancing Indian plate. In the Himalaya this stage is characterized by the intense uplift of the High Himalaya, the development of the Tibetan Plateau and the breaking-up of the central and eastern Asian continent. Although numerous models for the evolution of the Himalaya have been proposed, the available geological and geophysical data are consistent with an underthrusting model in which the Indian continental lithosphere underthrusts beneath the Himalaya and southern Tibet. Reflection profiles across the entire Himalaya and Tibet are needed to prove the existence of such underthrusting. Geodetic surveys across the High Himalaya are needed to determine the present state of the MCT as well as the rate of uplift and shortening within the Himalaya. Paleoseismicity studies are necessary to resolve the temporal and spatial patterns of major earthquake faulting along the segmented Himalayan mountains.  相似文献   

新变种矿物——铌铁锐钛矿及其共生矿物钕易解石     

黄婉康  郑巧荣  倪集众  王冠鑫 《矿物学报》1988,(1)

铌铁锐钛矿是含铌、铁的锐钛矿变种。呈土黄色、褐棕色,板状或土粒状。反射率589nm,15.9％,显微硬度H_v=275.9kg/mm~2。计算比重4.4g/cm~3。主要化学成分Nb_2O_534.92—44.3％,TiO_2 29.38—37.58％,Fe_2O_3 14.94—17.19％。化学式:(Ti_(0.44)Nb_(0.31)Fe_(0.25))_(1.00)O_2X射线分析表明该矿物属四方晶系,α=3.828±0.002,c=9.682±0.009,空间群I4_1/amd,Z=4。 共生矿物钕易解石,深红色者变生现象轻微;浅黄色钕易解石与铌铁锐钛矿可能形成于稍晚、较低温度条件下的矿化过程。  相似文献