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中强地震发震构造标志浅析——以2023年积石山M_(S)6.2地震为例
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作者 张军龙 徐岳仁 +1 位作者 李文巧 陈峰 《地震》 CSCD 北大核心 2024年第1期226-234,共9页
地震地表破裂是地震发生的重要特征,是研究地震动力学、构造变形的重要手段。一般认为,M6 3/4以上的地震才会形成地表破裂。但近年来,也有M6.0左右的地震发生了地表破裂。本文旨在探讨中强地震地表破裂的识别方法。中强地震发震构造的... 地震地表破裂是地震发生的重要特征,是研究地震动力学、构造变形的重要手段。一般认为,M6 3/4以上的地震才会形成地表破裂。但近年来,也有M6.0左右的地震发生了地表破裂。本文旨在探讨中强地震地表破裂的识别方法。中强地震发震构造的识别具有一定的挑战性,主要表现在以下几个方面:(1)中强地震地表破裂的规模(位错量、宽度、长度和深度)较小,容易被黄土层厚覆盖,掩盖地表破裂的痕迹,不易识别;(2)非构造成因裂缝干扰,使得难以区分构造成因地表破裂。本文以2023年积石山M_(S)6.2地震为例,对中强地震构造成因破裂的识别标志进行了初步分析,提出了以下识别标志:(1)地表破裂几何展布和剖面形态,地震伴生的次生灾害(滑坡、崩塌、砂土液化等)的线性分布为识别发震构造提供参考和线索;(2)地表破裂沿破裂走向呈现稳定地穿越不同地貌单元,至少穿越一条沟谷等低凹地貌;(3)地表破裂在地质剖面上表现出稳定的产状;(4)地表破裂伴生构造形态,地表沿破裂发育雁列式褶皱(挤压鼓包)与张裂缝交替出现的现象。本文提出的识别标志为中强地震发震构造的识别提供了新的思路。 展开更多
关键词 青藏高原 拉脊山断裂带 2023年积石山M_(s)6.2地震 发震构造 地震地表破裂
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A Comprehensive Bibliometric Analysis of China’s Free Trade Zones:Status and Evolutionary Trends
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作者 HUANG Lixia XU Miaoling 《Chinese Business Review》 2023年第3期127-140,共14页
The China free trade zone,crucial for advancing a new open economy,has gained significant attention lately.We analyzed 885 papers from Peking University Core and CSSCI journals(2012-2023)using CiteSpace for visualizat... The China free trade zone,crucial for advancing a new open economy,has gained significant attention lately.We analyzed 885 papers from Peking University Core and CSSCI journals(2012-2023)using CiteSpace for visualization.Our research results indicate that the literature on China’s free trade zone peaked with 171 articles in 2015,and gradually returned to an average of 45 articles per year.The main research focuses in this field include“institutional innovation”,“negative list”,“financial innovation”,“financial openness”,“opening up to the outside world”,and“economic growth”.In addition,cutting-edge analysis indicates that“dual circulation”and“blockchain”are future research trends.The main authors of the literature include Yang Bin,Zhu Xiaolin,Yuan Bo,Li Meng,Zhao Liang,and others.Their affiliated institutions,research institutes,and universities have not yet formed a clear core circle of authors;The top three research institutions with the highest number of publications are the International Trade and Economic Cooperation Research Institute of the Ministry of Commerce,Kaiyuan Law School of Shanghai Jiao Tong University,and the Comprehensive Research Institute of the Free Trade Zone of Sun Yatsen University.This article delves into the current hot topics and progress in the research of China’s free trade zones,providing important references and inspirations for future scholars in this field. 展开更多
关键词 China’s free trade zone bibliometric analysis CITEsPACE
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渤中8-4油田“S”型走滑转换带特征及其对浅层油气侧封的控制作用 被引量:1
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作者 黄志 杨海风 +4 位作者 江尚昆 张捷 赵昭 张震 于娅 《海洋地质前沿》 CSCD 北大核心 2024年第1期20-27,共8页
新构造运动在渤海海域表现强烈,形成了渤中凹陷特有的走滑构造体系和浅层油气藏。前人研究集中在走滑运动论证和走滑转换带类型探讨上,缺乏对走滑构造带控藏作用的精细研究。利用地震资料,结合油田实例,探讨了渤中8-4油田走滑转换带特... 新构造运动在渤海海域表现强烈,形成了渤中凹陷特有的走滑构造体系和浅层油气藏。前人研究集中在走滑运动论证和走滑转换带类型探讨上,缺乏对走滑构造带控藏作用的精细研究。利用地震资料,结合油田实例,探讨了渤中8-4油田走滑转换带特征和对油气侧封的控制作用。研究认为,渤中8-4油田主断裂为“S”型走滑转换带,发育释压带和增压带两类转换带。释压带地层陡,圈闭不发育,是油气由深向浅的充注段;增压带地层缓,背形特征清晰,低幅断鼻、断块圈闭集中发育,为油气汇聚区。建立了走滑断裂封闭指数以定量表征走滑转换带的侧封能力,通过近20个油田的统计分析,认为可以把走滑断裂封闭指数4作为走滑断层侧封的临界值。该成果为富砂背景下的浅层油气勘探工作提供了一种新的方法和思路。 展开更多
关键词 渤中西洼 走滑构造 s”型走滑转换带 控封作用
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2022年青海门源M_(S)6.9地震地表破裂带宽度调查与启示
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作者 牛鹏飞 韩竹军 +2 位作者 郭鹏 李科长 吕丽星 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2024年第2期548-570,共23页
地震地表破裂带是地震破裂在地表的直接表现,其宽度是活断层"避让带"和工程抗震设防重要的指示参数.无人机等测量手段的发展为获取地表破裂带的高分辨率影像数据、精细测量破裂带宽度、分析破裂带宽度空间分布特征以及限定合... 地震地表破裂带是地震破裂在地表的直接表现,其宽度是活断层"避让带"和工程抗震设防重要的指示参数.无人机等测量手段的发展为获取地表破裂带的高分辨率影像数据、精细测量破裂带宽度、分析破裂带宽度空间分布特征以及限定合理的活断层"避让带"提供了有利条件.2022年门源M_(S)6.9地震在青藏高原东北缘冷龙岭与托莱山断裂阶区部位产生了显著的左旋走滑型地表破裂带.基于震后获取的高精度无人机正射影像和数字高程模型,文中在门源地震地表破裂带全段精细解译的基础上,沿走向间隔100 m测量了251个宽度数据,R1破裂带最大宽度为209.78±14 m,平均宽度为42 m,R2破裂带最大宽度为115.31±15.72 m,平均宽度为26.14 m.宽度沿走向具有差异性,这主要受控于同震变形强度、破裂带几何结构以及地表第四系松散层发育状况;具体表现为同震位移量大、阶区等复杂几何结构以及穿过第四系松散层区段的破裂带比同震位移量小、平直段以及基岩区段的破裂带要宽.通过对去除离散值后的破裂带宽度数据统计分析,计算出95.4%和68.2%置信区间的有效宽度分别是70或50 m.在工程抗震设防中,若走滑型活断层评估的最大潜在震级与此次门源地震震级相近(~M 7.0),根据建(构)筑物类别,建议确定"避让带"宽度时参考本文获得的破裂带有效宽度(70或50 m).对于单一走滑型错动面发育地段,按建(构)筑物类别向两侧各扩展35或25 m即可;而对于活断层斜列阶区、平行断层围限区、走向弯曲区和双陡倾角错动面发育地段,在这些复杂几何结构分布范围的基础上需要各向两侧扩展35或25 m.本文研究结果可为建(构)筑物选址避让走滑型断层提供参考依据. 展开更多
关键词 走滑型地震 地震地表破裂带 活断层"避让带"宽度 门源M_(s)6.9地震 工程抗震设防
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2023年甘肃积石山M_(S)6.2地震对周围断层的应力影响及对余震的触发作用
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作者 周明月 万永革 +1 位作者 关兆萱 靳志同 《地震工程学报》 CSCD 北大核心 2024年第4期942-948,964,共8页
2023年12月18日,甘肃省临夏州积石山县发生M_(S)6.2地震,震中位于拉脊山断裂带。为深度剖析本次地震对周围断层和后续地震的静态库仑破裂应力影响,文章基于地震破裂模型参数和弹性半空间模型,计算积石山M_(S)6.2地震在周围主要断层上不... 2023年12月18日,甘肃省临夏州积石山县发生M_(S)6.2地震,震中位于拉脊山断裂带。为深度剖析本次地震对周围断层和后续地震的静态库仑破裂应力影响,文章基于地震破裂模型参数和弹性半空间模型,计算积石山M_(S)6.2地震在周围主要断层上不同深度产生的静态库仑破裂应力变化,并评估这些应力变化对未来地震危险性的影响。结果显示:本次地震使青海南山—循化南山断裂、拉脊山北缘断裂和拉脊山南缘断裂部分区域的库仑破裂应力显著增加,青海南山—循化南山断裂东段的库仑破裂应力增加远超出静态应力触发阈值,并达到了0.022 MPa,表现出较高地震危险性;其他断层也呈现出不同程度的库仑应力变化,拉脊山北缘断裂和拉脊山南缘断裂部分区域的应力卸载量达到了万帕,青海南山—循化南山断裂除东段外的其他分段和庄浪河断裂的应力卸载量达到了百帕。对不同震源深度下断层库仑破裂应力变化进行对比分析,发现深度变化对此次地震库仑破裂应力变化模式影响很大。文章还计算了本次地震在较大余震断层面上的库仑破裂应力,结果表明:甘肃积石山M_(S)6.2地震在后续三次M_(S)≥4地震的断层面上产生的库仑破裂应力分别为0.024 MPa、0.033 MPa和0.034 MPa,均超过触发阈值(0.01 MPa),表明M_(S)6.2地震对这三次地震具有明显的触发作用。文章可为该地区未来地震可能性与危险性的评估提供一定的参考。 展开更多
关键词 甘肃积石山M_(s)6.2地震 库仑破裂应力 地震危险性 拉脊山断裂带
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Chloride Resistance of Concrete under Complex Stress and Environment
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作者 Mohammed Saed Yusuf Xue Wen 《Open Journal of Civil Engineering》 CAS 2023年第1期171-180,共10页
The presence of stress is shown to have a significant impact on chloride ions in concrete. Reinforced concrete is usually durable and cost-effective which has resulted in its widespread use for construction, however, ... The presence of stress is shown to have a significant impact on chloride ions in concrete. Reinforced concrete is usually durable and cost-effective which has resulted in its widespread use for construction, however, the concrete subjected to environment and load has become increasingly apparently that attacked by aggressive agents such as chloride ion. In this study, the coupling influences are stress effects and environmental problems on the coastline concrete durability have been investigated. A series of cyclic of a wet-dry cycle and submersion tests were performed onto the stressed concrete to obtain an understanding of the physical mechanisms causing the accumulation of chlorides in the interior pores of concrete under different stress types and exposure environments, based on the same duration. Specimens were prepared and subjected to NaCl solution in a wet-dry cycle and submersion, the chloride in the tension zone is gradual with increasing the stress level, as well as the chloride ion in the wet-dry cycle, is increasing the number of cycles. The apparent diffusion coefficient of each specimen was calculated respectively, the profile of concentration at a different section of tension and compression zones were presented in influence factors of the number of cycles, the length of drying phase, and periodic wetting cycles with sodium solution was discussed. After employed Fick’s second law, the results suggested D<sub>a</sub> in a wet-dry cycle is much higher than the D<sub>a</sub> in submersion zones. 展开更多
关键词 Concrete Durability Chlorideion PENETRATION Wet Dry Cycle’s zone submerges zone Compressive stress Tensile stress Life Prediction MICRO-sTRUCTURE
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云南及邻区M_(S)≥6.0强震中短临动态跟踪综合预测方案
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作者 杨芬 《四川地震》 2024年第2期29-34,共6页
选取云南1992年1月至2021年8月应震效果通过R信度检验的11条地下流体前兆指标及2条地震学指标。利用数学模型对单项异常指标进行综合处理,并建立了预测阈值,为云南M_(S)≥6.0强危险区预测提供参考。利用分级预警模式建立了中期(T≤6个月... 选取云南1992年1月至2021年8月应震效果通过R信度检验的11条地下流体前兆指标及2条地震学指标。利用数学模型对单项异常指标进行综合处理,并建立了预测阈值,为云南M_(S)≥6.0强危险区预测提供参考。利用分级预警模式建立了中期(T≤6个月)和短临(T≤3个月)预测模型。通过研究1992年1月至2021年8月云南M_(S)≥6.0强震前小震空间活动特征,结果显示:M_(S)≥6.0强震危险区与强震前1~3年ML≥4.0地震有序活动区域相关,强震危险区位于或者邻近ML≥4.0地震有序活动区域;ML≥4.0地震有序活动呈现出围空、密集区和条带三种形式。 展开更多
关键词 云南及邻区 M_(s)≥6.0地震 综合预测 中短临预测 危险区预测
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2022年1月8日门源M_(S)6.9地震同震位移场及其发震断层形变破裂特征 被引量:3
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作者 李煜航 梁诗明 +9 位作者 郝明 葛伟鹏 李长军 宋尚武 张迎峰 华俊 陈俊先 梁洪宝 朱爽 甘卫军 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2023年第2期589-601,共13页
利用冷龙岭-托莱山断裂及其附近震前和震后GNSS观测资料,处理获取了2022年门源M_(S)6.9地震同震位移场,并以此为约束反演获取了地震同震破裂滑动分布图像,基于上述结果探讨了本次地震发震断层形变破裂特征,对比了区域震间与同震变形特征... 利用冷龙岭-托莱山断裂及其附近震前和震后GNSS观测资料,处理获取了2022年门源M_(S)6.9地震同震位移场,并以此为约束反演获取了地震同震破裂滑动分布图像,基于上述结果探讨了本次地震发震断层形变破裂特征,对比了区域震间与同震变形特征,结果表明:(1)此次地震在距震中约90 km范围内产生了10 mm及以上的同震永久变形,距震中160~200 km的GNSS连续站记录到的同震变形则十分微弱,总体在毫米级以下;(2)同震位移图像呈现典型的左旋走滑型同震变形模式.在距震中约3 km破裂带南侧的测站,其同震位移为近东向,大小445.9±3.3 mm,而在破裂带远场则呈现出典型的与左旋走滑型地震匹配的“四象限”对称分布的挤压或拉张尾端变形特征;(3)同震位移量以冷龙岭断裂-托莱山断裂为界,南北两盘具有明显的非对称性,南盘变形运动大于北盘;(4)托莱山断裂西段同震位移总体表现出随震中距减小而增大的“弹性回跳”现象,但其跨断层近场测站却并不服从上述同震变形特征,指示其并未参与此次地震破裂,考虑到托莱山断裂西段显著的左旋剪切应变能积累背景,其未来强震危险性值得关注. 展开更多
关键词 同震形变 2022年门源地震M_(s)6.9地震 祁连山活动构造带 GNss测量
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2021年9月16日四川泸县M_(S)6.0地震震区三维S波精细速度结构 被引量:2
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作者 吴萍萍 李大虎 +6 位作者 詹艳 郭慧丽 刘雪华 徐微 杨歧焱 鲁来玉 丁志峰 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2023年第6期2386-2403,共18页
近年来,四川盆地南缘(川南)中强地震频次增多和地震活动性增强,2021年9月16日四川省泸州市泸县M_(S)6.0地震的发生再次引起国内外学者对川南地区深部孕震环境和潜在地震危险性的密切关注.为了探究泸县6.0级地震震区的深部结构特征,本文... 近年来,四川盆地南缘(川南)中强地震频次增多和地震活动性增强,2021年9月16日四川省泸州市泸县M_(S)6.0地震的发生再次引起国内外学者对川南地区深部孕震环境和潜在地震危险性的密切关注.为了探究泸县6.0级地震震区的深部结构特征,本文基于最新布设于震区70个短周期密集地震台站的观测资料,采用背景噪声成像法构建了泸县M_(S)6.0震区三维S波精细速度结构.研究结果表明,研究区内喻家寺向斜和华蓥山断裂带东/西支深部速度结构表现明显非均匀性,喻家寺向斜构造区在深度3.0 km内表现为低速,随着深度增加,速度逐渐增大.华蓥山断裂带东、西支除了存在局部低速非均匀体,整体上表现为NE-SW展布的高速特征.泸县震源区西侧4.0~6.0 km深度呈现低速异常,东侧则表现高速异常分布,主震位于高低速分界带,震区周边存在大范围的明显线状几何特征的地震分布,震源深度优势分布层位主要集中在3.0~5.0 km之间.综合已有的资料分析,主震西侧的低速异常区指示着该处可能存在流体,推测泸县6.0级地震可能是在区域构造应力和流体扰动的作用下,泸县震区的先存隐伏断层发生错动所致. 展开更多
关键词 泸县地震 背景噪声成像 s波速度结构 华蓥山断裂带 孕震环境
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三亚M_(S)4.2地震前后海南岛重力场变化及其小波多尺度分解
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作者 李盛 黄章荣 +2 位作者 胡久常 解晓静 贾伟 《大地测量与地球动力学》 CSCD 北大核心 2023年第9期945-949,979,共6页
利用海南岛流动重力测网2016~2022年共13期复测资料,分析研究区域差分重力场和累积重力场动态变化,并着重分析2019-08-20海南三亚M_(S)4.2地震前后海南岛西南地区重力场时空变化。结果表明,三亚M_(S)4.2地震震中附近地区在震前2 a和3 a... 利用海南岛流动重力测网2016~2022年共13期复测资料,分析研究区域差分重力场和累积重力场动态变化,并着重分析2019-08-20海南三亚M_(S)4.2地震前后海南岛西南地区重力场时空变化。结果表明,三亚M_(S)4.2地震震中附近地区在震前2 a和3 a出现重力场累积变化梯度带,梯度带的异常范围约60 km,重力场变化最大约为60μGal;三亚M_(S)4.2地震之后,震中附近地区重力场继续上升,至2020年下半年才开始协同下降,在下降过程中,发生以2021-08-08乐东MS3.2地震为最大地震的震群事件。对2016-09~2019-08海南岛累积重力场动态变化小波多尺度分解表明,海南岛西南地区重力场变化在3阶、4阶和5阶小波细节图中均出现异常。 展开更多
关键词 三亚M_(s)4.2地震 重力场变化 梯度带 小波多尺度分解
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Geochemical characteristics and growth suitability assessment of Scutellaria baicalensis Georgi in the Earth's critical zone of North China 被引量:1
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作者 LI Xia WEI Xiao-feng +4 位作者 WU Jin YIN Zhi-qiang WAN Li-qin SUN Hou-yun AN Yong-long 《Journal of Mountain Science》 SCIE CSCD 2022年第5期1245-1262,共18页
Geochemical differentiation of soils has a series of consequences on plant and places pressure on the ecological environment.The quantitative evaluation of element migration in the Earth’s critical zone is a challeng... Geochemical differentiation of soils has a series of consequences on plant and places pressure on the ecological environment.The quantitative evaluation of element migration in the Earth’s critical zone is a challenging task.In this study,two demonstration study areas of Scutellaria baicalensis Georgi were selected,and multiple chemical weathering indexes,chemical loss fraction,mass migration coefficients and biological enrichment coefficient method were used to assess the ecological and geochemical suitability.The results show that for the element of Fe,Zn,Se,Cu,Co,Ni,Mo and Ge,the degree of weathering and soil maturation,were greater in the rhyolitic tuff area than in the Plagioclase gneiss area.In both research sites,the heavy metal level of samples in Scutellaria baicalensis Georgi did not exceed the standard limits.The plagioclase gneiss region’s surface soil environment was more alkaline,and the content of soil organic matter was lower,resulting in a higher bioenrichment intensity of Ge,Co,Cu,and Se elements in Scutellaria baicalensis Georgi than in the rhyolite-tuff area.The elements of Cd,Nb,Mo,Pb and As are considerably enriched in the soil of the plagioclase gneiss area but lost by leaching in the soil of the rhyolite tuff area,which is connected to the interplay of elemental abundance and human impact in the parent materials.This study provides a good example of how to assess growth suitability of Chinese medicinal materials in the Earth’s critical zone. 展开更多
关键词 Earth’s critical zone Biogeochemistry characteristics Weathering mechanism Element migration Chinese medicinal materials Chengde
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Crustal structure and accurate hypocenter determination along the Longmenshan fault zone 被引量:9
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作者 赵珠 范军 +2 位作者 郑斯华 长谷川昭 内茂木 《Acta Seismologica Sinica(English Edition)》 CSCD 1997年第6期66-73,共8页
A P and S wave velocity model is obtained for the crust in the region along the Longmenshan fault zone, Sichuan Province, China, by using data from a refraction profiling survey carried out in this region and those fr... A P and S wave velocity model is obtained for the crust in the region along the Longmenshan fault zone, Sichuan Province, China, by using data from a refraction profiling survey carried out in this region and those from local earthquakes. 202 local earthquakes along the fault zone are based on this velocity model, location errors being estimated to be about 1.5 km. The present relocations fairly improved the accuracy of hypocenter locations for earthquakes in this area, which is recognized from small scatter of data in the arrival time distance diagram compared with that for the original locations in the Earthquake Catalogue of Sichuan Seismic Network. The obtained hypocenter distribution shows that shallow earthquakes, confined to the upper crust in the depth range from 3 km to 22 km, are actively occurring along the main fault of the Longmenshan fault zone. The velocity model and the location method are presently used quite effective for precisely locating local earthquakes such as those in Sichuan Province. Installation of these with the real time processing system developed by Tohoku University in the Sichuan Telemetered Seismic Network would help to improve the location accuracy of events beneath the network. 展开更多
关键词 Longmenshan fault zone P wave s wave hypocenter determination velocity model arrive time curve
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Comparing mineral weathering and elemental transport between earth's critical zone with different parent rocks in Yanshan Mountain,Hebei province,China
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作者 Zijian Sun Zhen Liao +7 位作者 Wei Shen Daqing Fu Xiaofeng Wei Huiqiong Zhang Ziran Chen Lianghui Xiong Tianhao An Hao Wei 《Acta Geochimica》 EI CAS CSCD 2022年第6期982-999,共18页
Bedrock weathering performs a significant influence on the evolution of Earth’s critical zone.Carbonate rock(dolostone),metamorphic rock(gneiss),and sedimentary rock(sandstone)geological formations in Yanshan Mountai... Bedrock weathering performs a significant influence on the evolution of Earth’s critical zone.Carbonate rock(dolostone),metamorphic rock(gneiss),and sedimentary rock(sandstone)geological formations in Yanshan Mountain,Hebei Province,are taken as objects to probe the controlling of geological formations on weathering characteristics,migration,and enrichment of elements as well as structure of Earth’s critical zone under the identical climate conditions through geological field survey,analysis on minerals component,element distribution in the weathering profile.The dolostone geological formation(DGF)is lithologically dominated by dolostone,characterized by the strongest and predominant chemical weathering.During bedrock weathering and pedogenesis,DGF is marked by significant depletion of CaO,Mg O,S,Mn,Mo and enrichment of N,K,Fe_(2)O_(3),and Zn with concentrations of P,Cu,and B keeping stable.Shortage of soil-forming materials and significant loss are driven by soil erosion,which results in thin regolith and soil.The soil thickness is less than 10 cm,and the regolith thickness is less than 30 cm.The vegetation community is predominantly rock arbor or brush,which is calcivorous and tolerant of barrenness.Plagiogneiss is a dominant rock type of gneiss geological formation(GGF),characterized by the weakest weathering and fast chemical and physical weathering rate.GGF is masked by significant depletion of P,K,CaO,MgO,Fe_(2)O_(3),Mn,Cu and enrichment of N,S,Mo,and B,with contents of Zn keeping stable.Both soil and regolith developed in GGF are relatively thick for one of the reasons that biotite expands during weathering.The soil thickness is more than 50 cm,and the regolith thickness ranges from 100 to 200 cm.The vegetation community is predominantly high-quality economic forests and various arbors because of the enrichment of nutrients in GGF.Sandstone is primarily a rock type of sandstone geological formation(SGF),characterized by moderate weathering degree and slow chemical weathering rate.SGF is marked by significant depletion of P,K,CaO,MgO,Fe_(2)O_(3),and enrichment of N,S,Mn,Cu,Zn,and Mo,with fluctuant changes of Zn and B.The thickness of soil developed in SGF varies between that of DGF and GGF.The soil thickness ranges from 30 to 50 cm,and the regolith thickness ranges from 50 to 100 cm.Chinese pines are widely spread on the shady slopes of SGF.Research provides theoretical support for screening dominant ecological resource areas,ecological industry development and ecological protection and restoration for Yanshan Mountain,Hebei Province. 展开更多
关键词 Yanshan Mountain Earth’s critical zone Rock weathering PEDOGENEsIs Migration and enrichment of element
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Shanghai's Development Zones
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《China's Foreign Trade》 2008年第16期26-27,共2页
Since the early 1980s,development zones began appearing in Chi- na.Their success largely stems from the preferential policies they offer and the safe investment environment they work hard to cre- ate.As zones have per... Since the early 1980s,development zones began appearing in Chi- na.Their success largely stems from the preferential policies they offer and the safe investment environment they work hard to cre- ate.As zones have personalities themselves,it is essential to look beyond the pamphlets and published information and get down to the nitty- gritty.Shanghai has more State designated Economic and Technology De- velopment Zones than any other city in China.In the following article,we have chosen development zones... 展开更多
关键词 一刀 110 THAN shanghai’s Development zones
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Residual Stresses and Micro-Hardness Testing in Evaluating the Heat Affected Zone’s Width of Ferritic Ductile Iron Arc Welds 被引量:1
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作者 Georgios K. Triantafyllidis Dimitrios I. Zagliveris +5 位作者 Dionysios L. Kolioulis Christos S. Tsiompanis Titos N. Pasparakis Athanasios P. Gredis Melina L. Sfantou Ioannis E. Giouvanakis 《Materials Sciences and Applications》 2016年第1期73-82,共10页
Shielded Metal Arc Welding (SMAW) in Ductile Irons (DI) is often required by foundries for practical manufacturing reasons. The mechanical properties of the welded structures are strongly dependent on their HAZ’s wid... Shielded Metal Arc Welding (SMAW) in Ductile Irons (DI) is often required by foundries for practical manufacturing reasons. The mechanical properties of the welded structures are strongly dependent on their HAZ’s width. A model based on the behaviour of the ferritic matrix of high-Si DIs in order to make an approach in measuring their HAZ’s width is developed in this study. A series of thermal treatments on 3.35 and 3.75 wt% Si as-cast DIs and spot SMAWs is applied on these materials. The applied SMAWs are done on non-preheated and preheated samples (150℃ - 300℃). For welding we modify the amperage (100 - 140A). The micro-hardness Vickers changes in the ferrite of the as-cast samples and inside the HAZ of the welded ones can be attributed to the existence of residual stresses (RS) in the ferritic matrix and assist in estimating the HAZ’s width. 展开更多
关键词 WELDs Heat Affected zone Residual stresses Micro-Hardness Vickers Heat Affected zones Width
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2022年门源M_(S)6.9地震前祁连—海原断裂带闭锁程度及地震危险性研究 被引量:2
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作者 刘雷 朱良玉 +2 位作者 季灵运 庄文泉 刘传金 《地震研究》 CSCD 北大核心 2023年第1期88-98,共11页
利用2015—2021年GPS速度场,采用负位错程序反演祁连—海原断裂带的闭锁程度及滑动亏损速率,结合断层面小震分布特征研究2022年门源M_(S)6.9地震震前异常特征,综合分析该断裂带各段的地震危险性,并根据跨断层GPS剖面获取断裂带滑动速率... 利用2015—2021年GPS速度场,采用负位错程序反演祁连—海原断裂带的闭锁程度及滑动亏损速率,结合断层面小震分布特征研究2022年门源M_(S)6.9地震震前异常特征,综合分析该断裂带各段的地震危险性,并根据跨断层GPS剖面获取断裂带滑动速率,对区域地壳变形特征进行探讨。结果表明:在2022年门源地震前,冷龙岭断裂处于强闭锁状态,并且闭锁深度在15 km,滑动亏损速率也较大,小震分布也相对较少,这些特征与中强地震的发生密切相关。而金强河断裂、冷龙岭断裂西段和托莱山断裂东段现今闭锁程度较高,闭锁深度深,滑动亏损速率大,具有较高的地震危险性。进一步结合小震分布和2022年门源地震前闭锁特征,认为未来需关注托莱山东段的中强地震危险性。祁连—海原断裂带现今走滑速率为3.9~4.3 mm/a,说明该断裂带整体运动一致性较好,挤压速率从西段的2.9 mm/a向东逐渐减小为1 mm/a,说明青藏高原东北缘现今的地壳形变主要以祁连山上的地壳短缩和祁连—海原断裂带上的左旋走滑运动为主。 展开更多
关键词 祁连—海原断裂带 门源M_(s)6.9地震 断层闭锁 地震危险性 地壳变形
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利用接收函数两步反演法研究小江断裂带及邻区地壳S波速度结构
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作者 杨建文 金明培 +2 位作者 茶文剑 张天继 叶泵 《地震地质》 EI CSCD 北大核心 2023年第1期190-207,共18页
文中基于2011年9月2日—2014年1月16日小江断裂带及邻区48个台站的远震三分量波形数据提取径向P波接收函数,采用两步反演法和Bootstrap重采样技术反演了各台站下方的S波速度结构,对小江断裂带及邻区的地壳深部结构进行了研究。结果表明... 文中基于2011年9月2日—2014年1月16日小江断裂带及邻区48个台站的远震三分量波形数据提取径向P波接收函数,采用两步反演法和Bootstrap重采样技术反演了各台站下方的S波速度结构,对小江断裂带及邻区的地壳深部结构进行了研究。结果表明:1)研究区地壳的S波速度在横向和垂向上都存在明显的非均匀特性,近地表处有2~4km厚的低速沉积层;中上地壳的S波速度呈高、低速相间分布;在20~35km的深度范围内存在明显的低速层,主要间断分布于小江断裂以西的川滇菱形块体和红河断裂以南的印支块体内部,另外在师宗-弥勒断裂附近也有局部分布。2)小江断裂带中、北段壳内低速层较为发育,以中段最为突出,最厚约达28km;南段在15~25km深度范围内存在明显的高速区。3)研究区的泊松比普遍较低(平均为0.24),呈不均匀分布,且横向变化剧烈,小江断裂带的泊松比总体呈北段较高、南段次之、中段低的分段特征;研究区壳内低速分布与泊松比间的对应关系不明显,大部分低速层似乎缺少发生部分熔融的条件,其地球物理结果的差异和不一致说明壳内低速层的变形演化机制及物理特性较为复杂。 展开更多
关键词 小江断裂带 P波接收函数 两步反演法 s波速度 中下地壳低速层
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Exploring China's (Shanghai) Pilot Free Trade Zone ra——the "Negative List" Mode
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作者 Wang hua 《Review of Global Academics》 2014年第5期369-370,共2页
China (Shanghai) pilot free trade zone (FTZ)formally approved by the state council on August 22, 2013, was officially opened on September 29. It is the important measures to comprehensiw',ly deepen reforms and op... China (Shanghai) pilot free trade zone (FTZ)formally approved by the state council on August 22, 2013, was officially opened on September 29. It is the important measures to comprehensiw',ly deepen reforms and open still wider to the outside world in China. Exploring "pre-establistnnent national treatment" and "negative list" management mode is a feature of the free trade zone of Shanghai, which is adapt to economic globalization, to win the international competition o fthe initiative a qualitative leap. 展开更多
关键词 s'.aanghai free trade zone negative list pre-establishment national treatment
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Report on China's First Economic Development Zone for Poverty Relief
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《China Today》 1997年第6期60-61,共2页
关键词 Report on China’s First Economic Development zone for Poverty Relief
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Development Tendency of China's Special Economic Zones
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《China's Foreign Trade》 2000年第10期9-10,共2页
关键词 Development Tendency of China’s special Economic zones
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