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| 1 | Structural pattern of eastern Himalayan syntaxis in Namjagbarwa and its formation process显示文摘The structural pattern of the eastern Himalayan syntaxis in Namjagbarwa consists of two series of structures with different styles. One series compiles the earlier ductile contractional and lateral-slip deformation system, formed by nearly north-south shortening within the syntaxis, left-lateral and right-lateral slipping along its western and eastern boundaries respectively. They were possibly produced by the indentation of the Indian continent into Asian continent after India-Asia collision. The peak deformation-metamorphic ages in these structures are 62-60 Ma, ~23 Ma and ~13 Ma. The other series is composed of ductile-brittle normal faults distributing concentrically and dipping toward the outsides of Namjagbarwa Peak. They were probably the collapse structures caused by rapid uplift in a later time and the beginning ages for the normal faulting are about 7.3-6.3 Ma. | ZHANG Jinjiang, Jl Jianqing, ZHONG Dalai, DING Lin & HE Shundong1. Department of Geology, Peking University, Beijing 100871, China 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Correspondence should be addressed to Zhang Jinjiang (email: zhjj@pku.edu.cn) | 2004 | Science China Earth Sciences2004，47，2： | 34 |
| 2 | Structure and deformation around the Gyirong basin, north Himalaya, and onset of the south Tibetan detachment system显示文摘Gyirong basin and its adjacent area are located at a special position in the Himalayan orogen, where the south Tibetan detachment system (STDS) and N-S trending rift converged. The north Himalayan orogen here can be divided into five petrologic-tectonic units successively from south to north: 1) the Greater Himalayan crystalline complex (GHC); 2) the STDS shear zone; 3) the Tethyan Himalayan sedimentary sequence (THS); 4) the late Cenozoic sedimentary basins, such as Gyirong and Oma basins; and 5) the Malashan gneiss dome. Structural studies show that this area experienced four stages of deformation: 1) the earlier south-directed thrusting, preserved both in the GHC and THS; 2) top-down-to-north slip along the STDS, normal faults related to this slip formed the early controlling structures of the Cenozoic basins,and the tilted pattern of the blocks between the basins indicated a north-directed slip; 3) east-west extension, the resultant N-S trending normal fault formed the eastern boundary of the basins; and 4) late gravitational collapse. Zircon SHRIMP U-Pb dating on the syn-deformational (leuco-) granite along the STDS indicates that the major activity of the STDS occurred at ca. 26 Ma, but its onset may have begun as early as ca. 36 Ma. | YANG XiongYing ZHANG JinJiang QI GuoWei WANG DeChao GUO Lei LI PengYuan LIU Jiang | 2009 | Science China Earth Sciences2009，52，8： | 33 |
| 3 | Fault-tolerant Control Systems-An Introductory Overview显示文摘This paper presents an introductory overview on the development of fault-tolerant control systems. For this reason, the paper is written in a tutorial fashion to summarize some of the important results in this subject area deliberately without going into details in any of them. However, key references are provided from which interested readers can obtain more detailed information on a particular subject. It is necessary to mention that, throughout this paper, no efforts were made to provide an exhaustive coverage on the subject matter. In fact, it is far from it. The paper merely represents the view and experience of its author. It can very well be that some important issues or topics were left out unintentionally. If that is the case, the author sincerely apologizes in advance.After a brief account of fault-tolerant control systems, particularly on the original motivations, and the concept of redundancies, the paper reviews the development of fault-tolerant control systems with highlights to several important issues from a historical perspective. The general approaches to fault-tolerant control has been divided into passive, active, and hybrid approaches. The analysis techniques for active fault-tolerant control systems are also discussed. Practical applications of faulttolerant control are highlighted from a practical and industrial perspective. Finally, some critical issues in this area are discussed as open problems for future research/development in this emerging field. | JinJiang | 2005 | 自动化学报2005，31，1： | 30 |
| 4 | Structural and Geochronological Evidence for Multiple Episodes of Tertiary Deformation along the Ailaoshan-Red River Shear Zone, Southeastern Asia, Since the Paleocene显示文摘结构的分析证明 Ailaoshan 红的河剪碎带(ASRRSZ ) inAilao 山由三不同 deformational domaias 组成。这些领域可以代表三个事件左侧面滑倒由 ASRRSZ 富有经验。如此的变丑的第一个事件在 transtensional 政体下面在整个 ASRRSZ 的东方高级的带发生了并且生产了角闪岩等级的 L 类型侦探棉火药。第二个事件左侧面滑动形成的高度套印高级的带的火车地区。它的 deformational 机制类似于 simples 听见并且使变形的岩石是绿色片岩等级的 L-S 糜棱岩。第三个事件 ofleft 侧面滑倒在 ASRRSZ 的一条西方的低档带主要发生了。这变丑在 transpressional 政体发生了,形成了一个左首的戳系统的一个全面结构模式并且生产了 low-greenschist 等级的 phyllonltes。Geochronological 数据显示三个事件左侧面滑倒发生在近似 58-56 妈前,至少从约 27 妈 to22 妈并且在近似 13-12 妈分别地。第一个事件在 ASRRSZ 滑倒看起来在 -60 对应于印度和亚洲的起始的碰撞妈。第二个事件几乎在象最集中的压缩的一样的时间发生了并且在西藏高举。最近的事件可能在近似 16-13 妈后面在西藏代表进一步东方的材料流动。因此,东南的亚洲的 ASRRSZ 可能经历了三个主要事件第三级左侧面自从印度亚洲碰撞,在 intracontinental 集中期间滑倒。 | ZHANG Jinjiang ZHONG Dalai SANG Haiqing ZHOU Yong | 2006 | Acta Geologica Sinica(English Edition)2006，80，1： | 27 |
| 5 | Multistage Extension and Age Dating of the Xiaoqinling Metamorphic Core Complex,Central China显示文摘There are two extensional systems in the Xiaoqinling metamorphic core complex (XMCC). One is the detachment fault system developed along the peripheries of the XMCC, which extended in an ESE-WNW direction and whose upper plate moved towards the WNW. The other extensional system includes the retrograde shear zones and normal faults developed within the XMCC, which represent the collapse of the XMCC. Ar-Ar and K-Ar dating shows that the extension of the detachment fault system continued from 135 to 123 Ma, i.e. in the late stage of its evolution at about 127 Ma. The collapse represented by the extensional system within the XMCC was operative during 120-106 Ma, and its main activity occurred about 116 Ma ago. These suggest that the XMCC experienced two extensional stages in its evolution, i.e., the syn-orogenic regional extension and post-orogenic collapse extension. | ZHANG Jinjiang ZHENG Yadong | 1999 | Acta Geologica Sinica(English Edition)1999，73，2： | 22 |
| 6 | Application of General Shear Theory to the Study of Formation Mechanism of the Metamorphic Core Complex:A Case Study of Xiaoqinling in Central China显示文摘The kinematic vorticity number and strain of the mylonitic zone related to the detachment fault increase from ESE to WNW along the moving direction of the upper plate of the Xiaoqinling metamorphic core complex (XMCC) and the geometry of quartz c-axis fabrics changes progressively from crossed girdles to single girdles in the same direction. Therefore, pure shear is dominant in the ESE part of the XMCC while simple shear becomes increasingly important towards WNW. However, the shear type does not change with the strain across the shear zone, thus the variation of shear type is of significance in indicating the formation mechanism. The granitic plutons within the XMCC came from the deep source and their emplacement was an active and forceful upwelling prior to the detachment faulting. The PTt path demonstrates that magmatism is an important cause for the formation of the XMCC. The formation mechanism of the XMCC is supposed to be active plutonism and passive detachment. Crustal thickening and magmatic | ZHANG Jinjiang ZHENG Yadong LIU Shuwen | 2000 | Acta Geologica Sinica(English Edition)2000，74，1： | 20 |
| 7 | Strain and kinematic vorticity analysis:An indicator for sinistral transpressional strain-partitioning along the Lancangjiang shear zone,western Yunnan,China显示文摘This work deals with the preliminary relationship between strain path and strain partitioning pattern in a sinistral transpressional zone,Lancangjiang shear zone,located to the southeast of Tibet.Various ductile rocks provide an opportunity to investigate quantitative finite strain(Rs),kinematic vorticity values(Wm),and proportions of simple and pure shear components.The mean kinematic vorticity values(Wm) were evaluated based on three methods,such as Rs-θ,prophyroclast hyperbolic distribution method(PHD),and polar Mohr diagram construction(PMD).Wm for mylonitic metasediments of the low-grade schist belt ranged from 0.19 to 0.54.Protomylonites,mylonites,and ultramylonites recorded differential Wm values,0.19―0.73,0.11―0.8,and 0.84―0.95(even 0.99) respectively in the high-grade gneiss belt.Based on classical strain analysis and these kinematic vorticity evaluations,the shear zone is classified as a preliminarily bulk monoclinic symmetry.The pattern of vorticity path suggests that a previously undocumented transpressional setting and strain partitioning pattern in the southeast region of Tibet Plateau,characterized by steep-narrow domain of simple-shearing(Tertiary strike-slip shearing) deformation and wider domain of mostly pure-shearing(Tertiary contraction) to accommo-date intracontinental deformation. | Bo Zhang JinJiang Zhang DaLai Zhong Lei Guo | 2009 | Science China Earth Sciences2009，52，5： | 16 |
| 8 | Structural characteristics of middle and southern Xainza-Dinggye Normal Fault System and its relationship to Southern Tibetan Detachment System显示文摘The Xainza-Dinggye Normal Fault System (XDNFS) is a large-scale nearly-north-south trending exten-sional structure across central and southern Tibet. Its middle segment developed in Tethys Himalaya with features of earlier magmatic core complex and later normal faults dipping moderately to northwest-west. The magmatic core complex is made up by mylonitic leucogrante with a low-angle detachment fault on the top of it and overlain by lower-grade meta-sedimentary rocks. The structural pattern of the southern segment of XDNFS take the shape of a detachment fault dipping to southeast-east with the High-Himalayan rock series as the lower plate. The Southern Tibetan Detachment System (STDS) is expressed as a ductile shear zone composed of mylonitic leucogranite in the studied area of this note. STDS was cut by the later XDNFS, which presents that nearly-east-west striking STDS is not the controlling or adjusting structure of the nearly-north-south trending ex-tensional structures. The origin of | ZHANG Jinjiang GUO Lei DING Lin | 2002 | Chinese Science Bulletin2002，47，13： | 16 |
| 9 | Orogen-parallel extension in Himalaya: Is it the indicator of collapse or the product in process of compressive uplift?显示文摘Extensional structures developed extensively in Himalaya with their strikes perpendicular to that of the orogenic belt. The studies of such structures in Qusum, Burang, Lhozhag, Nyalam and Yadong show that they represent an orogen-parallel extension. The basins produced by the extension experienced orokyn-perpendicular compression during their formation. The ages of the extension rang from 16 to 13 Ma and coincide with the intensive compressive stage in Southeastern Asia. Therefore, the extension is Syn-shortening and the dominate tectonic movement in Himalaya was compression and uplift during the extension. The extension was the partition of compressive deformation rather than the indicator for the collapse and falling of the Tibetan Plateau. | ZHANG Jinjiang, DING Lin, ZHONG Dalai & ZHOU Yong Institute of Geology and Geophysics. Chinese Academy of Sciences. Beijing 100029, China | 2000 | Chinese Science Bulletin2000，45，2： | 16 |
| 10 | Mineral chemistry, P-T-t paths and exhumation processes of mafic granulites in Dinggye, Southern Tibet显示文摘The mafic granulites in Dinggye, as various scale lense-shaped enclaves within the high Himalayan crystalline rock series, occur along mylonitic foliations at the junction between the Southern Tibetan Detachment System (STDS) and the Xainza-Dinggye normal fault system. The main lithological assemblage comprises garnet plagioclase pyroxenite, garnet two-pyroxene granulite, pyroxene garnet amphibolite and so on. The detailed petrological analyses show that these mafic granulites underwent at least four-stage metamorphic evolution. The first metamor-phic stage, the garnet+clinopyroxene+quart mineral assemblage (M1) was probably formed un-der eclogite facies, the second stage, the plagioclase+clinopyroxene symplectite mineral as-semblage (M2) was produced under high-pressure granulite facies by the early decompressive breakdown of M1 mineral assemblage, the third stage, the plagioclase+clinopyroxene+ hypersthene symplectite mineral assemblage (M3) was formed at granulite facies by the late period decompressive breakdown of M1 and M2 mineral assemblages and the final stage, pla-gioclase+hornblende mineral assemblage (M4) was formed by hydrolysis of earlier mineral as-semblages during late uplifting. The detailed mineral composition analyses suggest that garnets and clinopyroxenes within M1 and M2 mineral assemblages display similar compositions to the equivalents in the B and C types of eclogites, whereas the M3 clinopyroxenes are akin to these of the same kind of minerals in the granulite. These mineral chemistry features and P-T estimates calculated by mineral thermometers and barometers indicate that the early stage relic porphyro-blasts (M1) could be formed at the eclogite facies, the early decompressive breakdown (M2) occurred at the high-pressures granulite facies of 1.35―1.48 GPa and 625―675℃, the M3 mineral assemblage recorded the granulite facies of 0.7―0.95 GPa and 775―900℃ and M4 plagioglase+hornblende retrograde mineral assemblage was produced under the amphibolite facies metamorphism with pressure of 0.4 to 0.75 GPa and temperature at between 660 and 700℃. These construct P-T paths from crustal subduction overthickening to tectonic uplift tectono-thermal evolution. The mineral chemical characteristics and P-T condition at every metamorphic stage of these granulites indicate that these rocks experienced the eclogite facies metamorphism during the early stage. Subsequently, these mafic granulites underwent the three-stage exhuma-tion of the eclogite facies tectonic uplift, isostatic uplift related to the transformation from ec-logite/high-pressure granulite to granulite facies and extensional uplift. | LIU Shuwen ZHANG Jinjiang SHU Guiming LI Qiugen | 2005 | Science China Earth Sciences2005，48，11： | 13 |
| 11 | Dryland Expansion in Northern China from 1948 to 2008显示文摘This study examines the expansion of drylands and regional climate change in northern China by analyzing the variations in aridity index(AI), surface air temperature(SAT), precipitation and potential evapotranspiration(PET) from 1948 to 2008.It is found that the drylands of northern China have expanded remarkably in the last 61 years. The area of drylands of the last 15 years(1994–2008) is 0.65 × 106km2(12%) larger than that in the period 1948–62. The boundary of drylands has extended eastward over Northeast China by about 2° of longitude and by about 1° of latitude to the south along the middleto-lower reaches of the Yellow River. A zonal band of expansion of semi-arid regions has occurred, stretching from western Heilongjiang Province to southern Gansu Province, while shifts to the east of semi-arid regions in dry subhumid regions have also occurred. Results show that the aridity trend of drylands in northern China is highly correlated with the long-term trend of precipitation and PET, and the expansion of semi-arid regions plays a dominant role in the areal extent of drylands, which is nearly 10 times larger than that in arid and subhumid regions. | LI Yue HUANG Jianping JI Mingxia RAN Jinjiang | 2015 | Advances in Atmospheric Sciences2015，32，6： | 12 |
| 12 | Structural feature and its significance of the northernmost segment of the Tertiary Biluoxueshan-Chongshan shear zone,east of the Eastern Himalayan Syntaxis显示文摘Here we describe ductile,ductile-brittle and brittle deformation styles in the northern segment of the Tertiary Biluoxue-shan-Chongshan shear zone lying to the east of the Eastern Himalayan Syntaxis.In the northernmost part of the zone in the vicinity of the Eastern Himalayan Syntaxis,it consists of mylonitic gneiss,granite,and schist.Based on field relations andmineral assemblages,the rocks are classified into gneiss belt in the west limb,including banded gneiss,augen mylonite and migmatite gneiss,and schist belt in the east limb.Except for the massive granite pluton,the other three tectonites are affected by polystage deformation (D1-D4).Fold deformation of the first stage D1 is isoclinal to tight pattern with nearly N-S fold axes and steeply axial planar cleavage S1,which resulted in the local crustal thickening under a contractive setting.D2 overprinted D1 and is characterized by tight folds with steep axes and N-S fold axial planar,which are also characterized by large-scale ductile strike-slip shear foliation S2,parallel to the nearly N-S trending axial planes of D1 and D2.The structural pattern of D2 represents a transpression along the zone.D3 occurred during the late stage of the transpression or post-transpression,produc-ing the NW-SE and NE-SW trending strike-slip faults of the third stage D3.Following the D3 deformation,the zone was ex-humed to shallow crustal level where the various tectonites underwent a brittle transtensional deformation D4,combined with one N-S trending strike-slip component and one normal faulting component.Structures and previous geochronologies presented in the paper suggest that the study area is correlated with those in the adjacent tectonic zones,Ailaoshan-Red River shear zone and Gaoligong shear zone in the western Yunnan.It underwent intensive polyphase deformation,namely,crustal thickening,transpression,and transtension,responding to syn-collision and post-collision of India-Eurasia from 65 Ma to current period east of the Eastern Himalayan Syntaxis. | ZHANG Bo ZHANG JinJiang ZHONG DaLai WANG XiaoXian QU JunFeng GUO Lei | 2011 | Science China Earth Sciences2011，54，7： | 11 |
| 13 | THE NP-HARDNESS OF THE SINGLE MACHINE COMMON DUE DATE WEIGHTED TARDINESS PROBLEM显示文摘In this paper we prove that the single machine common due dateweighted tardiness problem is NP-hard. | YUAN Jinjiang (Department of Mathematics,Zhengzhou University,Zhengzhou 450052,China) | 1992 | Systems Science and Mathematical Sciences1992，5，4： | 10 |
| 14 | Structures of Syn-deformational Granites in the Longquanguan Shear Zone and Their Monazite Electronic Microprobe Dating显示文摘The Longquanguan shear zone is an important structural belt in the North China Craton, separating the underlying Fuping complex from the overlying Wutai complex. This shear zone has experienced three episodes of deformation: the first and main episode is a ductile top-to-ESE shear along the gently northwest-west dipping foliations, while the other two episodes are later collapse sliding. Prolonged granites parallel to the shear foliations make one of the main compositions of the Longquanguan shear zone. These granites experienced deformation to form mylonitic rocks when they emplaced during the first episode of deformation. Structural characters of the granites and their contacts to the country rocks indicate that these granites possibly resulted from in-situ partial re- melting by shearing, i.e., they are syn-deformational granites. Monazites in these mylonitic granites are magmatic minerals and their crystallization ages may represent ages of the magmatic events, and also the ages for the main deformation of the Longquanguan shear zone. Monazite electronic microprobe dating were carried on two samples of granite, which gives multiple peak ages, among which 1,846 Ma and 1,877 Ma are the main peak ages for the two samples. These ages represent the main deformation of the Longquanguan shear zone, which is consistent with the main regional geological event at about 1,850 Ma caused by the collision between the Eastern and Western Blocks in North China. The good match between the monazite ages and the corresponding regional tectono-thermal events shows the feasibility and reliability of monazite electronic microprobe dating. | ZHANG Jinjiang*, ZHAO Lan and LIU Shuwen The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education School of Earth and Space Sciences, Peking University, Beijing 100871 | 2006 | Acta Geologica Sinica(English Edition)2006，80，6： | 9 |
| 15 | Middle-Miocene transformation of tectonic regime in the Himalayan orogen显示文摘Understanding the multiple tectonic transformations during the Himalayan orogeny is significant in evaluating the evolution of Himalayan orogen.In the Gyirong area in south Tibet,deformed leucogranitic veins in the biotite-plagioclase gneisses of Greater Himalayan crystalline complex(GHC) constitute south-vergent asymmetric folds.The reconstruction of the veins shows that they experienced two generations of deformation under different tectonic regimes:an earlier top-to-north extension and a later top-to-south thrusting,implying a tectonic transformation from N-S extension to N-S shortening.Zircons LA-ICP-MS U-Pb dating of the leucogranite shows that it was emplaced during 21.03-18.7 Ma.The data suggest that the tectonic transformation occurred after 18.7 Ma.The chronological data of South Tibet detachment system(STDS) and North-South trending rift(NSTR) from Gyirong and other areas indicate that the Himalayan orogeny was in a period of tectonic transformation from N-S extension to N-S shortening during 19-13 Ma.The transformation of tectonic regime was probably controlled by the India-Asia convergence rate.An increase in the convergence rate resulted in N-S shortening of the orogen,thrusting and folding,with coeval formation of the NSTR in Tibet.A decrease in the convergence rate led to N-S extension and reactivation of the STDS. | WANG XiaoXian ZHANG JinJiang LIU Jiang YAN ShuYu WANG JiaMin | 2013 | Chinese Science Bulletin2013，58，1： | 8 |
| 16 | Mesozoic thrusts and extensional structures in the Daqingshan orogen, Inner Mongolia, and their temporal and spatial relationship显示文摘三大规模戳在 Daqingshan orogen 发展了,内部蒙古,与东北东方,到 Suletu 的从 Louhuashan 的 trending 在这篇论文被描述。这些指导西北的戳,和四条构造的带(或构造的表) 由这些差错分开了,形成了一个典型推进系统。原来定义的 Hohhot 变形核心建筑群可以是一张构造的表,做推进的系统的最高的构造联合起来并且在顶上由 Daqingshan 分开差错截断了。存在 tectono 按年代先后的研究证明可能推进这个区域沿着最高的分开差错发生在象延期的一样的时间。这在 Daqingshan orogen 的收缩和延期可能是同时的礼品。Daqingshan orogen 的结构的模式能为同时的推进被相关到喜玛拉雅的 orogen,和模型,在 Himalaya 的分开可以为解释 Daqingshan orogen 的发展给一个提示。 | QI Guowei ZHANG Jinjiang WANG Xinshe GUO Lei | 2007 | Progress in Natural Science:Materials International2007，17，2： | 6 |
| 17 | DEGREE CONDITIONS OF INDUCED MATCHING EXTENDABLE GRAPHS显示文摘A simple graph G is induced matching extendable,shortly IM\|extendable,if every induced matching of G is included in a perfect matching of G .The degree conditions of IM\|extendable graphs are researched in this paper.The main results are as follows:\;(1) 2n/32n/32n/32n/3 is the minimum integer δ such that every graph with minimum degree at least δ is IM\|extendable,where n=|V(G)|≥6 is even.\;(2) is the minimum integer δ such that every graph with minimum degree at least δ is IM\|extendable,where n=|V(G)|≥6 is even.\;(2) (2n-2)/3 is the minimum integer k such that, for k′≥k ,every k ′ regular graph with vertex number n is IM\|extendable,where n=|V(G)| is even, n ≥8 and n ≠10. | Liu Yan\ Yuan Jinjiang\ Wang Shiying Dept.ofSystem Sci.and Math.,Zhengzhou Univ.,Zhengzhou 450052 | 2000 | Applied Mathematics(A Journal of Chinese Universities)2000，15，1： | 6 |
| 18 | Structures,kinematics,thermochronology and tectonic evolution of the Ramba gneiss dome in the northern Himalaya显示文摘The Ramba gneiss dome,one of the north Himalayan gneiss domes,is composed of three tectono-lithologic units separated by an upper and a lower detachment fault.Low-grade metamorphic Tethyan Himalayan sedimentary sequence formed the upper unit above the brittle upper detachment fault.Mylonitic gneiss and a leucogranite pluton made up the lower unit beneath the ductile lower detach- ment fault.Mylonitic middle-grade garnet-,staurolite-and andalusite-schist constituted the middle unit between the two faults,which may be that the basal part of the upper unit experienced detachment shear.The Ramba dome underwent three episodes of deformation in its tectonic evolution.The first episode was a top-down-to-north-northwest sliding possibly related to the activity of the south Tibetan detachment system(STDS).The second episode was the dominant deformation related to a east–west extension,which resulted in a unique top-down-to-east kinematics and the major tectonic features of the dome.The third episode was a collapse sliding toward the outsides of the dome.The Ramba gneiss dome is possibly a result of the east–west extension and magmatic diapir.The lower detachment fault is probably the main detachment fault separating the sedimentary sequence from the crystalline basement during the east–west extension in the dominant deformation episode.The diapir of the leucogranite pluton formed the doming shape of the Ramba gneiss dome.This pluton intruded in the core of the dome in a late stage of the dominant deformation,and its Ar–Ar cooling ages are about 6 Myr.This indicates that the dominant deformation of the dome happened at the same time of the east–west extension represented by the north–south trending rifts throughout the northern Himalaya and southern Tibet.Therefore,the formation of the Ramba gneiss dome should be related to this east–west extension. | Lei Guo Jinjiang Zhang Bo Zhang | 2008 | Progress in Natural Science:Materials International2008，18，7： | 6 |
| 19 | Dual roles of Hh signaling in the regulation of somatic stem cell self-renewal and germline stem cell maintenance in Drosophila testis显示文摘 | ZhaoZhang XiangdongLv JinJiang LeiZhang YunZhao | 2013 | Cell Research2013，23，4： | 6 |
| 20 | A challenge to the concept of slip-lines in extrusion tectonics显示文摘门户大开塑造 V 结合在亚洲的差错典型地与挤出 tectonics 有关的罢工滑倒。然而,构造模型基于粘性的滑倒线理论把一些批评问题与它联系了。conjugate 在飞机变丑滑倒线设定,根据粘性的理论应该对每另外一个,但是,事实上正常在conjugate 罢工滑倒差错之间的角度,在东方地中海在挤出 tectonics 被认为是滑倒线,西藏中间亚洲,中国和印度支那半岛的区域,总是是超过 | Yadong Zheng Erchie Wang Jinjiang Zhang Tao Wang | 2011 | Geoscience Frontiers2011，2，1： | 6 |
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