|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | A comparative study of natural and experimental nano-sized grinding grain textures in rocks显示文摘In three shallow-level fault systems in eastern China, nano-sized (30―100 nm) grinding grain textures are found in the thin-shelled rheological layer representing frictional-viscous high strain field. The surface layer near slipping plane is composed of stacks of grinding grains with high sphericity and uniform nano-sized diameter, while the underlying layer appears as a mixture of irregular ones with diverse diameters. Rock deformation experiments indicate that the grinding grain texture is a common phenomenon in shearing fractures, suggesting a potential transition from sliding friction to rolling one during the rock deformation process. This transition is crucial for many tribological processes in geo- logical fields. | SUN Yan SHU LiangShu LU XianCai LIU Hao ZHANG XiHui K. KOSAKA LIN AiMing | 2008 | Chinese Science Bulletin2008，53，8： | 13 |
| 2 | Relationship between Landslides and Active Normal Faulting in the Epicentral Area of the AD 1556 M~8.5 Huaxian Earthquake,SE Weihe Graben(Central China)显示文摘In this paper, we focus on the characteristics of the landslides developed in the epicentral area of AD 1556 M^8.5 Huaxian Earthquake, and discuss their relations to the active normal faults in the SE Weihe Graben, Central China. The results from analyzing high-resolution remote-sensing imagery and digital elevation models(DEMs), in combination with field survey, demonstrate that:(i) the landslides observed in the study area range from small-scale debris/rock falls to large-scale rock avalanches;(ii) the landslides are mostly developed upon steep slopes of ≥30°; and(iii) the step-like normal-fault scarps along the range-fronts of the Huashan Mountains as well as the thick loess sediments in the Weinan area may facilitate the occurrence of large landslides. The results presented in this study would be helpful to assess the potential landslide hazards in densely-populated areas affected by active normal faulting. | Gang Rao Yali Cheng Aiming Lin Bing Yan | 2017 | Journal of Earth Science2017，28，3： | 10 |
| 3 | 岩石剪切面纳米粒子层的近期研究进展显示文摘20世纪90年代,在各类岩石剪切面中相继发现纳米级和微米级超微粒子结构,近期结合力学、物理学成因研究又有新的进展.在超微观上,通过国内外的实例实测,从岩石剪切面纳米粒子层赋存展布的普遍性,结构特征的层次性,成因机制的非线性和功能效应的多样性四个方面,进行简要阐述,萃取更多信息.进而初步揭示了剪切摩擦黏性发育与纳米粒子形成间的共生关系,和剪切运动中岩石的分离、分凝和分层作用首先由纳米粒子层的滑移启动开始的.并分析了岩石塑性流变实质上是超微粒子(纳米-微米级磨粒)的运动,以及岩石剪切面纳米粒子层一些特殊的物理和化学地质作用等.诚然,纳米粒子层蕴涵的信息是丰富的,该项研究还处于起步开拓阶段,仅试图为构造地质学和相关学科领域提出新的理念和新的探讨平台. | 孙岩 舒良树 陆现彩 刘浩 Aiming Lin K.Kosaka | 2007 | 自然科学进展2007，17，10： | 8 |
| 4 | 构造地球化学研究展望显示文摘以断裂构造地球化学为主,从常量元素-微量元素-稀土元素及其分异耗散顺序;矿物脉体-次生包裹体-同变形期流体及其微观动力学分析;压力强度-温热梯度-溶液浓度及其耦联相关体系;构造应力场-流变物理场-地球化学场及其参量数字模拟等4方面研究展望。上述4个方面既自成系统又相互关联,在时空演化上,可以结合地球动力学、构造年代学等统一解释。 | 孙岩 朱文斌 郭继春 刘德良 Aiming Lin | 2002 | 自然科学进展2002，12，9： | 8 |
| 5 | Recent progress in studies layer in rock on the nano-sized particle shear planes显示文摘Since the 1990s, an ultramicro-particle texture in nano- or micron-sized scale has been continually found in shear planes of various rocks, and recently further progress was made in generic physical mechanisms. In this article, the characteristics of the nano-sized particle layer in rock shear planes (including widespread distribution, layering texture, non-linear genetic mechanism, and multiple functions) on an ultra micro-scale were briefly introduced and more information was obtained by analyzing cases from home and abroad. Our findings suggest that (1) there is a paragenetic relationship between the development of shear frictional- viscous and the formation of nano-sized particles, and (2) in the shear movement, partitioning, segregating, and layering in rocks are initiated by the sliding motion of the nano-sized particle layer. Moreover, the plastic rheology of rocks is essentially the move- ment of ultra-micro-sized particles (nano-size and micro-size), and the nano-sized particle layer in rock shear planes is characterized by some particular physical and chemical effects. | Yan Sun Liangshu Shu Xiancai Lu Hao Liu Xihui Zhang Aiming Lin Kazuo Kosaka | 2008 | Progress in Natural Science:Materials International2008，18，4： | 7 |
| 6 | 变质岩透入性面理的纳米结构研究显示文摘通过江西变质岩透入性面理滑移面扫描电子显微镜(SEM)4例观测,发现其表面普遍存在纳米粒子层状结构,并为三轴压力实验所验证.在剪切滑移过程中纳米颗粒(直径φ40~95nm)经过粒化-异化-分化,个体形态有别,结构层次分明.这个纳米界限薄膜(层),本质上是具有黏-弹性变形的摩擦-黏性(frictional-viscous)带.在此微域条带中,构造应力场-流变物理场-地球化学场非常活跃,并同变质岩面理发育3个阶段(剪切滑移强化作用-弱化作用-易剥作用)密切关联.进而可从黏-弹性变形行为揭示构造剪切的微观运动学机理. | 孙岩 陆现彩 Xihui Zhang 刘浩 Aiming Lin | 2009 | 中国科学(D辑)2009，39，8： | 5 |
| 7 | Nano-texture of penetrative foliation in metamorphic rocks显示文摘By observing four samples obtained from Jiangxi Province, China, under the scanning electron mi-croscope (SEM), we discovered that nano-particle layers were commonly formed on sliding planes of the penetrative foliation in metamorphic rocks. We also successfully reproduced this phenomenon with a tri-axial pressure experiment. Having gone through the granulitization-alienation-partition in the shear sliding process, the nano-particles (40-95 nm in diameter) display different individual shapes and dis-tinct layered textures. This nano-confinement layer is essentially a frictional-viscous stripe with vis-cous-elastic deformation. In the micro-domain stripe, activities in structural stress field-rheological physical field-geochemical field are very dynamic, corresponding to the three stages (i.e., shear sliding strengthening-weakening-exfoliating) of the foliation development in metamorphism rocks. As such, the viscous-elastic deformation behavior helps shed light on the understanding of the micro-dynamic mechanism of the structural shearing. | SUN Yan LU XianCai ZHANG XiHui LIU Hao LIN AiMing | 2008 | Science China Earth Sciences2008，51，12： | 5 |
| 8 | 剪切滑动带断层岩中超微结构的实例观测和研究展望显示文摘通过SEM观测,在三例韧脆性剪切滑动带的断层岩(美国加利福尼亚州Cajon Pass深钻中的变余糜棱岩,陕北陕参1井和黄海NH钻中的流变岩)中,发现了韧脆性剪切带断层岩所特有的微米纳米级超微磨粒结构.从微粒组构学、粒滑流变学、叶理岩相学和微观动力学(包括动热变质作用、流体渗散作用和颗粒自旋作用)等几个方面,拟对磨粒结构蕴藏的丰富地质信息进行扼要简述,从而展示这一新领域探讨的问题和前景. | 孙岩 陆现彩 舒良树 顾连兴 朱文斌 郭继春 Aiming Lin | 2005 | 自然科学进展2005，15，1： | 3 |
| 9 | Coulomb Stress Evolution History as Implication on the Pattern of Strong Earthquakes along the Xianshuihe-Xiaojiang Fault System, China显示文摘Coulomb stress accumulation and releasing history and its relationship with the occurrence of strong historical earthquakes could deepen our understanding of the occurrence pattern of strong earthquakes and hence its seismic potential in future. The sinistral strike-slip Xianshuihe-Xiaojiang fault zone(XXFS) is one of the most dangerous fault zones in China, extending 1 500-kmlong from the central Tibetan Plateau to the Red River fault zone. There are 35 M≥6.5 historical earthquakes occurred since 1327, hence it is an ideal site for studying the Coulomb stress evolution history and its relationship with the occurrences of strong earthquakes. In this study, we evaluated the Coulomb stress change history along the XXFS by synthesizing fault geometry, GPS data and historical earthquakes. Coulomb stress change history also revealed different patterns of historical earthquakes on different segments of the XXFS, such as characteristic recurrence intervals along the Salaha-Moxi fault and super-cycles along the Xianshuihe fault. Based on the occurrence pattern of past historical earthquakes and current Coulomb stress field obtained in this study, we suggest positive ΔCFS and hence high seismic potential along the Salaha-Moxi fault and the Anninghe fault. | Bing Yan Shinji Toda Aiming Lin | 2018 | Journal of Earth Science2018，29，2： | 3 |
| 10 | Detection of Variants of B.1.617 Lineage from Five Returning Chinese Nationals at a Guangxi-Vietnam Border Port——Guangxi Zhuang Autonomous Region,China,April 2021显示文摘A 47-year-old male(Patient A)passenger from Vietnam whose nucleic acid results for coronavirus disease 2019(COVID-19),also known as severe acute respiratory syndrome coronavirus 2(SARS-CoV-2),were positive at Pingxiang Customs on April 29,2021,and subsequently confirmed by Guangxi CDC laboratories on April 30. | Ning Kang Yinpin Liu Fuyin Bi Jing Wang Huafeng Chen Jing Wang Zhenli Liang Min Chen Guangwu Wei Aiming Li Yonghong Li Bao Lu Zhenling Jiang Yi Tan Ge Zhong Mei Lin Yu Ju | 2021 | China CDC weekly2021，3，30： | 3 |
| 11 | Late Holocene activity and historical earthquakes of the Qiongxi thrust fault system in the southern Longmen Shah fold-and-thrust belt,eastern Tibetan Pla-teau显示文摘 | Wang M M Jia D Lin Aiming | 2013 | Tectonophysics2013，584，： | 1 |
| 12 | Tectonic characteristics of the central segment of the Tancheng-Lujiang fault zone, Shandon Peninsula, eastern China显示文摘 | Lin Aiming Miyata T Wan Tianfeng | 1998 | Tectonophysics1998，293，： | 1 |
| 13 | Singularityanalysis of three-legged parallel robots based onpassive-joint velocities显示文摘 | YANG Guilin CHEN Aiming LIN Wei | 2001 | IEEE Transactions onRobotics and Automation2001，17，4： | 1 |
| 14 | Roundness of clasts in pseudotachylytes and cataclastic rocks as an indicator of frictional melting显示文摘 | Aiming Lin | 1999 | Journal of Structural Geology1999，，5： | 1 |
| 15 | Late Quaternary right-lateral displacement along active faults in the Yanqi Basin, southeastern Tianshan, northwest China显示文摘 | Lin Aiming Fu Bihong Kano Ken-ichi | 2002 | Tectonophysics2002，354，34： | 1 |
| 16 | How and when did the Yellow river develop its square bend显示文摘 | Lin Aiming YangZhenyu SunZhiming | 2001 | Geology2001，29，10： | 1 |
| 17 | Tectonic Cha-racteristics of the Central Segment of the Tancheng -Lujiang Fault Zone, Shangdong Peninsula,EasternChina显示文摘 | Lin Aiming Miyata T Wan Tianfeng | 1998 | Tectonophysics1998，293，： | 1 |
| 18 | How and when did the Yellow River develop its square bend显示文摘 | Lin Aiming Yang Zhenyu Sun Zhiming | 2001 | Geology2001，29，10： | 1 |
| 19 | Late Quaternary right- lateral displacement along active faults in the Yanqi Basin, southeastern Tian Shan, Northwest China显示文摘 | Lin Aiming Bihong Fu Ken-ichi Kano | 2002 | Tectonophysics2002，354，： | 1 |
| 20 | Catalytic ozonation of phenol in water with natural brucite and magnesia显示文摘 | Kun HE Yuming DONG Lin YIN Aiming ZHANG Zhen LI | 2006 | Chinese Journal Of Geochemistry2006，25，B08： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员