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| 1 | Contemporary crustal movement of continental China obtained by global positioning system(GPS) measurements显示文摘We obtain a unified horizontal velocity field of continental China and vicinity through measurements at 81 GPS stations provided by the National Key Infrastructure Project, Crustal Movement Observation Network of China. The velocity field delineates patterns of movements and deformation of active crustal blocks in continental China under the Eurasia-fixed reference frame. The space-based geodesy also clearly shows for the first time the horizontal movementand deformation of continental China induced by indentation of the Indian plate. The data provide kinematic constraints for simulating dynamic process of continental litho-spheric deformation. | MA Zongjin, CHEN Xinlian, YE Shuhua, LAI Xian, WEI Ziqing, CHEN Junrong, NING Jinsheng, XU Huoze & DING Guoyu1. Insitute of Geology, China Seismological Bureau, Beijing 100029, China (e-mail: disgroup@publi.bta.net.cn)2. Center for Analysis and Prediction, China Seismological Bureau, Beijing 100036, China 3. Shanghai Astronomic Observatory, Chinese Academy of Sciences, Shanghai 200030, China 4. Institute of Seismology, China Seismological Bureau, Wuhan 430077, China 5. Institute of Survey and Mapping, Xi’an 710054, China 6. National Bureau of Survey and Mapping, Beijing 100830, China 7. Wuhan University, Wuhan 430077, China 8. Institute of Geodesy and Geophysics, Wuhan 430077, China 9. China Seismological Bureau, Beijing 100036, China | 2001 | Chinese Science Bulletin2001，46，18： | 34 |
| 2 | Structural Analysis of the Multi-layer Detachment Folding in Eastern Sichuan Province显示文摘像梳子、像马槽的褶层的一个连续剧在东方四川发展了,由合拢的多层的分开控制了,与在他们的发展的古典 Jura 类型结构不同。导致这些结构的发展的关键因素是在到学习区域的中生代地层学的 Neoprotozoic 的不同部分的分开层的出现,它,从底部到顶,是 Banxi 组,的更低的部分更低寒武纪( Niutitang 形成),更低的志留纪( Longmaxi 形成和 Luoreping 形成),上面二叠( Wujiaping 形成)并且更低三叠纪( Daye 形成)。根据与沙箱建模相结合的领域调查,这研究主张 Banxi 组的更低的部分的分开层控制了像梳子的褶层的发展,并且寒武纪的分开层的更低的部分控制了像马槽的褶层的发展。因为发生在学习区域的几分开层,双结构的发展不同规模是重要变丑机制,并且 duplexes 是与合拢结构的典型分开区分开来的重要结构。由于这些 duplexes,表面结构和结构的高度不能是深入地的结构的高度。同时,分开层是为有益于累积的理解的油 / 气体移植和油和气体的移植的好隧道。 | WANG Zongxiu ZHANG Jin LI Tao XIE Guoai MA Zongjin | 2010 | Acta Geologica Sinica(English Edition)2010，84，3： | 12 |
| 3 | Experimental study on mechanical behaviors of pseudo-ductile cementitious composites under biaxial compression显示文摘Experimental investigation was conducted to characterize the responses of pseudo-ductile cementitious composites (PDCCs) when subjected to uniaxial and biaxial compression.The PDCCs is a class of fiber reinforced cementitious composites with ultra-high ductility by using a low volume fraction (2%) of polyvinyl alcohol (PVA) fiber.Two different strength grades of PDCC were examined with cubic specimen size of 100 mm in the tests.The specimens were loaded with a servo-hydraulic jack at different stress ratios.The principle stresses and strains of the specimens were recorded,and the failure modes with various stress states were examined.The test results indicated that the ultimate strength of PDCCs increased due to the lateral confinement in the other principal stress direction,and the maximum ultimate strength occurred at the biaxial stress ratio of 0.25,which was very different from common concrete material.For the PDCC specimens,the biaxial strength may be lower than the uniaxial strength when subjected to biaxial compression with the stress ratio of 1.0,and the failure mode showed a shear-type failure because of the bridging effect of fibers.Finally,a failure criterion was proposed for PDCCs under biaxial compression. | ZHOU JiaJia PAN JinLong LEUNG Christopher Kin Ying LI ZongJin | 2013 | Science China(Technological Sciences)2013，56，4： | 8 |
| 4 | The uplifting process of the Bogda Mountain during the Cenozoic and its tectonic implication显示文摘The Tianshan Mountains have undergone its initial orogeny, extension adjusting and re-orogeny since the Late Paleozoic. The re-orogeny and uplifting process of the orogeny in the Mesozoic and Cenozoic are two of most important events in the geological evolution of Euro-Asian continent, which resulted in the formation of the present range-and-basin pattern in topography of the Tianshan Mountains and its adjacent areas. Thermochronology results by the method of fission-track dating of apatite suggest three obvious uplifting stages of the Bogad Mountain Chain re-orogeny during the Cenozoic, i.e. 5.6-19 Ma, 20-30 Ma, and 42-47 Ma. The strongest uplifting stage of the mountain is the second one at 20 -30 Ma, when the mountain uplifted as a whole, and the beginning of re-orogeny was no less than 65 Ma. Furthermore, our studies also show that the uplifting types of the mountain are variable in the dif-ferent time periods, including uplifting of mountain as a whole and differential uplifting. The apparently diversified uplifting processes of the mountain chain are characterized by the migration (or transfor-mation) of the uplifting direction of the mountain from west to east and from north to south, and the main process of mountain extending is from north to south. | ZongXiu Wang Tao Li Jin Zhang YongQing Liu ZongJin Ma | 2008 | Science China Earth Sciences2008，51，4： | 8 |
| 5 | Hyperbolic Method to Analyze the Electrical Resistivity Curve of Portland Cements with Superplasticizer显示文摘Electrical measurement was employed to investigate the early hydration characteristics of cement pastes with different dosages of superplasticizer in the same W/C ratio.The hyperbolic method was applied to analyze the electrical resistivity development.The peak point(P_h)on the hyperbolic curve could be easily read.The time(th)to reach the point Ph had strong relations with the setting time.th was delayed with the increment of the dosage of superplasticizer.The time th was used to plot the relationship between the initial setting time and final setting time.The hyperbolic equation was established to predict the ultimate resistivity. The retardation effect of the superplasticizer was confirmed in the same W/C ratio by setting time and isothermal heat evolution. | WEI Xiaosheng XIAO Lianzhen LI Zongjin | 2008 | Journal of Wuhan University of Technology(Materials Science)2008，23，2： | 7 |
| 6 | Multistage Deformation in the Northeastern Segment of the Jiangshao Fault (Suture) Belt: Constraints for the Relationship between the Yangtze Plate and the Cathaysia Old Land显示文摘Multistage deformation events have occurred in the northeastern Jiangshao Fault (Suture) Belt. The earliest two are ductile deformation events. The first is the ca. 820 Ma top-to-the-northwest ductile thrusting, which directly resulted from the collision between the Cathaysia Old Land and the Chencai Arc (?) during the Late Neoproterozoic, and the Jiangnan Orogenic Belt that formed as the ocean closed between the Yangtze Plate and the jointed Cathaysia Old Land and the Chencai Arc due to continuous compression. The second is the ductile left-lateral strike-slipping that occurred in the latest Early Paleozoic. Since the Jinning period, all deformation events represent the reactivation or inversion of intraplate structures due to the collisions between the North China and Yangtze plates during the Triassic and between the Philippine Sea and Eurasian plates during the Cenozoic. In the Triassic, brittle right-lateral strike-slipping and subsequent top-to-the south thrusting occurred along the whole northeastern Jiangshao Fault Zone because of the collision between the North China and Yangtze plates. In the Late Mesozoic, regional extension took place across southeastern China. In the Cenozoic, the collision between the Philippine Sea and Eurasian plates resulted in brittle thrusts along the whole Jiangnan Old land in the Miocene. The Jiangshao Fault Belt is a weak zone in the crust with long history, and its reactivation is one of important characteristics of the deformation in South China; however, late-stage deformation events did not occur beyond the Jiangnan Old Land and most of them are parallel to the strike of the Old Land, which is similar to the Cenozoic deformation in Central Asia. In addition, the Jiangnan old Land is not a collisional boundary between the Yangtze Plate and Cathaysia Old Land in the Triassic. | ZHANG Jin LI Jinyi XIAO Wenxia FENG Qianwen MA Zongjin | 2013 | Acta Geologica Sinica(English Edition)2013，87，4： | 7 |
| 7 | Meso-Cenozoic Evolution of the Tanlu Fault and Formation of Sedimentary Basins显示文摘There are a group of large and medium-scale Meso-Cenozoic petroliferous basins along both sides of the Tanlu fault or within the fault zone, e.g., the Songliao basin, the Bohai Bay basin and the Subei-Yellow Sea basin. As shown by studies of the structural types, sedimentary formations, volcanic activities, tectonic evolution as well as the time-space relationship between the Tanlu fault zone and the basins, the formation and distribution of the basins are controlled by the movement of the Tanlu fault. This paper presents an analysis of the tectono-geometric, kinematic and geodynamic features of the basins on the basis of integrated geological-geophysical data, and an exploration into the internal relations between the fault and the basins as well as the formation mechanism and geodynamic processes of the basins. | WANG Weifeng JIN Qiang MA Zongjin | 1998 | Acta Geologica Sinica(English Edition)1998，72，4： | 5 |
| 8 | Structural Traces of Secondary Faults(Fractures) along the Main Faults and Their Reliability as Kinematic Indicators显示文摘Secondary/minor structures occurring along the main fault surfaces are important indicators for judging the kinematic characteristics of faults.However,many factors can lead to the formation of these structures,which results in the difficulty for rapid judgment and application in the fields.A series of secondary faults/fractures developed due to the movement of main faults are the most important and widespread phenomena in the scope of brittle deformation.The morphology of the main fault surfaces is vari... | Jin ZHANG Jinyi LI Zongjin MA Wenjun REN | 2011 | Acta Geologica Sinica(English Edition)2011，85，5： | 5 |
| 9 | Infrared Spectroscopy Study of Structural Nature of Geopolymeric Products显示文摘The bonding status and chemical environment of SiO 4 and AlO 4 tetrahedras of three types of geopolymeric products were systematically investigated by infrared spectroscopy.The relationship between amorphous geopolymeric products and zeolite crystals with the same overall chemical compositions was also discussed.The infrared evidence shows that SiO 4 tetrahedra is partially bonded by AlO 4 during the hydration process of geopolymeric cement.The two types of tetrahedras jointly construct the three dimensional framework structures of the geopolymeric products.The mutual transformation between geopolymeric products and corresponding zeolite crystals will take place once the reaction condition is suitable,which reveals that the nature of geopolymeric products are probably the amorphous equivalent of the corresponding zeolite crystals. | ZHANG Yunsheng SUN Wei LI Zongjin | 2008 | Journal of Wuhan University of Technology(Materials Science)2008，23，4： | 4 |
| 10 | Human embryonic stem cells-derived endothelial cell therapy facilitates kidney regeneration by stimulating renal resident stem cell proliferation in acute kidney injury显示文摘Endothelial cell therapy has been implicated to enhance tissue regeneration and vascularization in ischemic kidney. However, no published study has yet examined direct effects of endothelial cell treatment in kidney recovery. This study investigated the therapeutic efficacy of endothelial cells in a mouse model with acute kidney injury (AKI). Thus, human embryonic stem cells-derived endothelial cells (hESC-ECs) labeled with a reporter system encoding a double fusion reporter gene for firefly luciferase (Fluc) and green fluorescent protein (GFP) were characterized by Fluc imaging and immunofluoresence staining. Cultured hESC-ECs (1×106) were injected into ischemic kidney shortly after AKI. Survival of the transplanted hESC-ECs was monitored in vivo from day 1 to 14 after endothelial cell transplantation and potential impact of hESC-EC treatment on renal regeneration was assessed by histological analyses. We report that a substantial level of bioluminescence activity was detected 24 h after hESC-EC injection followed by a gradual decline from 1 to 14 d. Human ESC-ECs markedly accelerated kidney cell proliferation in response to ischaemia-induced damage, indicated by an elevated number of BrdU+ cells. Co-expression of Sca-1, a kidney stem cell proliferation marker, and BrdU further suggested that the observed stimulation in renal cell regeneration was, at least in part, due to increased proliferation of renal resident stem cells especially within the medullary cords and arteriole. Differentiation of hESC-ECs to smooth muscle cells was also observed at an early stage of kidney recovery. In summary, our results suggest that endothelial cell therapy facilitates kidney recovery by promoting vascularization, trans-differentiation and endogenous renal stem cell proliferation in AKI. | JIA XiaoHua L He LI Chen FENG GuoWei YAO XinPeng MAO LiNa KE TingYu CHE YongZhe XU Yong LI ZongJin KONG DeLing | 2013 | Chinese Science Bulletin2013，58，23： | 4 |
| 11 | Study on the transverse structures across Taiwan Strait显示文摘The mountain ranges are almost NE- or NNE-trending in mainland and Taiwan island across the strait. But a number of correspondent transverse structures across Taiwan Strait have been identified on the basis of morphology, surface structure, deep seismic survey and gravity field etc. Moreover, it is inferred from the square or/and rectangular shape of the isoseist maps of 8 M≥6 earthquakes occurring in the western foothill plain of Taiwan that there is an apparent segmentation of the Taiwan Island along the N-S orientation. This has been verified from the GPS's results of the ground motions measured during the Chi-Chi earthquake in 1999. As a matter of fact, the transverse structures within the Taiwan Island could be correlated with more salient NW- and EW-trending structures in the mainland of Fujian than in Taiwan. The investigation of the transverse structures across Taiwan Strait is conducive to realizing the geology within the strait. Hence, the tectonic sketch map of the strait as well as mainland and island drawn in this context shows NW- and EW-trending structures for the study area. | MA Zongjin (马宗晋) WANG Chien-Ying (王乾盈) XU Jie (徐杰) NIE Fengjun (聂逢君) ZHANG Jin (张进) | 2002 | Science China Earth Sciences2002，45，12： | 4 |
| 12 | Preparation of Metakaolin Based Geopolymer and Its Three-dimensional Pore Structural Characterization显示文摘Three types of pure geopolymer pastes(poly-sialate PS, poly- sialate-siloxo PSS, and polysialate-siloxo PSDS) were fi rst prepared by alkali(Na OH and KOH) activated metakaolin. Then a void space network was employed to simulate the 3-D pore-throat distribution across the unit cell of the various hardened geopolymer pastes with reference to their experimental mercury intrusion curves. Based on the simulated 3-D pore-throat structure models, a wide range of pore-level properties such as porosity, connectivity, permeability and tortuosity of various geopolymer pastes were calculated. The 3-D structural model and calculated parameters showed that most of the pores in Na-PS geopolymer paste was very small size pores ranging from 0 to 100 nm. A few very large pores were spread amongst the small pores, resulting in a very high penetration pressure, permeability resistance. Unlike Na-PS geopolymer paste, pore size with medium size of Na-PSS, K-PS and K-PSS geopolymer pastes distributed uniformly across the unit cell, and the size changes of adjacent pores in the 3 geopolymer pastes were little, producing higher penetration pressure, lower permeability, smaller connectivity and larger tortuosity. In contrast, pores in Na-PSDS and K-PSDS geopolymer pastes were relatively large and distributed concentratively, which caused samples to be easily penetrated by mercury, methane and nitrogen etc under relatively low pressures. | 张云升 ZHANG Wenhua SUN Wei LI Zongjin LIU Zhiyong | 2015 | Journal of Wuhan University of Technology(Materials Science)2015，30，3： | 3 |
| 13 | Structural Traps in Detachment Folds:a Case Study from the 'Comband Trough-like' Deformation Zone/s,East Sichuan,China显示文摘Detachment structures occur widely in the crust,and it is the commonest and most important deformation type developed in the region between orogenic belts and basins.The ’comb-like’ and ’toughlike’ fold belts in eastern Sichuan are caused by multi-layer detachment.The duplex structure is the most important deformation style in the region,exhibiting different characteristics from typical detachment structures.Different deformation styles,scales,and shortenings resulting from independent deformations of various detachment systems would lead to the phenomenon whereby most of the topographical heights in the region do not correspond to the structural heights in depth.Based on systematic structural analysis and combined with practical oil/gas prospecting,four types of structural traps are described from eastern Sichuan Province,which are:detachment and thrust trap;detachment folding trap;fault-flat blocking trap;and detachment layer trap.Meticulous studies on the deformation and distribution of detachment layers in the eastern Sichuan Province will contribute to oil/gas prospecting and selection of potential regions of marine-origin oil/gas prospecting in South China. | WANG Zongxiu ZHANG Jin LI Tao ZHOU Xingui MA Zongjin TANG Liangjie XIAO Weifeng YAN Xili | 2012 | Acta Geologica Sinica(English Edition)2012，86，4： | 3 |
| 14 | Basement Structure and Properties of the Western Junggar Basin, China显示文摘A comprehensive geophysical profile stretching from Qingyijing at the southern edge of the Junggar Basin to Ubara on the northern margin of the Junggar Basin was conducted in an attempt to probe the crustal structure of the western Junggar Basin(hereafter referred to simply as ‘the Basin'), and, in particular, the structure and property of the Basin's crystalline basement. A survey using seismically converted waves was conducted along this profile to determine the characteristics of the P-and Swave velocities typical of the crust and uppermost mantle. A joint inversion of gravitation and aeromagnetic data was also performed to acquire the density and magnetization intensity values found beneath the western Basin. This research revealed that the Basin is composed of the so-called Manasi terrain in the south, and the Wulungu terrain in the north. Their boundary is located along the WNW-trending Dishuiquan-Sangequan suture, linking the NE-striking Da'erbute suture(DS) in the west, and the WNWtrending Kalameili suture(KS) in the east. In its northern part, the Wulungu-type terrain has a doublelayered basement, of which the upper layer is a folded basement of Hercynian orogenic origin, and the lower layer is a crystalline basement of Middle–Upper Proterozoic age. The southern part of the Basin, i.e., the Manasi terrain, has a single-layered crystalline basement. The folded basement here is too thin to be clearly distinguished. | Junmeng Zhao Shuze Chen Gong Deng Xuezhong Shao Heng Zhang Jamshed Aminov Xinfa Chen Zongjin Ma | 2019 | Journal of Earth Science2019，30，2： | 3 |
| 15 | Quantitative Characterization and Elastic Properties of Interfacial Transition Zone around Coarse Aggregate in Concrete显示文摘Backscattered electron images(BSE) obtained by scanning electron microscope was used to quantitatively characterize the microstructure of interfacial transition zone(ITZ) in concrete. Influences of aggregate size(5, 10, 20, and 30 mm), water to cement ratio(0.23, 0.35 and 0.53) and curing time(from 3d to 90d) on the microstructure of interfacial transition zone between coarse aggregate and bulk cement matrix were investigated. The volume percentage of detectable porosity and unhydrated cement in ITZ was quantitatively analyzed and compared with that in the matrix of various concretes. Nanoindentation technology was applied to obtain the elastic properties of ITZ and matrix, and the elastic modulus of concrete was then calculated based on the Lu & Torquato model and self-consistence scheme by using the ITZ thickness and elastic modulus obtained from this investigation. The experimental results demonstrated that the microstructure and thickness of ITZ in concrete vary with a variety of factors, like aggregate size, water to cement ratio and curing time. The relative low elastic properties of ITZ should be paid attention to, especially for early age concrete. | 贾子健 HAN Yunge 张亚梅 QIU Chen HU Chuanlin LI Zongjin | 2017 | Journal of Wuhan University of Technology(Materials Science)2017，32，4： | 2 |
| 16 | Molecular cloning, tissue expression and protein structure prediction of the porcine 3-hydroxy-3-methylglutaryl-coenzyme A reductase ( HMGR ) gene显示文摘 | Xiao Chen Xiaofeng Wang Zongjin Li Lujun Kong Guifen Liu Jinluan Fu Aiguo Wang | 2011 | Gene2011，，2： | 2 |
| 17 | Some Fundamental Problems of Geodynamics and Application of Earth Observations by Space-Based Measurements显示文摘Although great-progress has been made in the earth sciences,some fundamental problems of geodynamics remain unsolved.They are concerned with the whole earth as well as regional tectonics,such as the west Pacific and Qinghai-Xizhang plateau.The new generation of earth observation by space-based measurement will contribute to solving these problems of geodynamics.In this regard,some specific plans about application of these techniques are suggested in this paper. | Ma Zongjin,Zhang Peizhen,Hong Hanjin,and Gao Xianglin Institute of Geology,SSB,Beijing 100029,China | 1997 | Earthquake Research in China1997，11，1： | 2 |
| 18 | Effect of aggregates and water contents on the properties of magnesium phospho-silicate cement显示文摘 | Zhu Ding Zongjin Li | 2004 | Cement and Concrete Composites2004，，1： | 2 |
| 19 | Pressure retardation of organic maturation in clastic reservoirs:A case study from the Banqiao Sag,Eastern China显示文摘 | Li Huijun Wu Tairan Ma Zongjin | 2004 | Marine and Petroleum Geology2004，21，9： | 1 |
| 20 | Fabrication and piezoelectricity of 0-3 cement based compos- ite with nano-PZT powder显示文摘 | LI Zongjin GONG Hongyu ZHANG Yujun | 2009 | Current Applied Phys- ics2009，9，3： | 1 |
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