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| 1 | Surface Rupture and Co-seismic Displacement Produced by the Ms 8.0 Wenchuan Earthquake of May ^(12)th,2008,Sichuan,China:Eastwards Growth of the Qinghai-Tibet Plateau显示文摘女士 8 的地震给 Wenchuan 以县,西方的四川,中国,在 2008 年 5 月 12 日并且导致了长表面破裂(> 300 km ) 。关于表面破裂的第一手的观察在 Yingxiu, Beichuan 和 Qingchuan 的最糟点击的区域由地震生产了,查明地震的原因的结构在 Longmenshan 构造的带的中央差错地区。沿着 Yingxiu-Beichuan 破裂地区活动范围 2.5-4 m 的单个差错的平均 co 地震的垂直排水量和越过中央、正面的 Longmenshan 差错的累积垂直排水量系上带子是大约 56 m。表面破裂力量从 Beichuan 的北方被归结为 Qingchuan 县和表演 23 m 右罢工滑倒部件。Wenchuan 指责戳的地震是在印度、欧亚的大陆的连续集中的行动下面的西藏的高原的东方生长的表明。 | DONG Shuwen ZHANG Yueqiao WU Zhenhan YANG Non MA Yinsheng SHI Wei CHEN Zhengle LONG Changxin AN Meijian | 2008 | Acta Geologica Sinica(English Edition)2008，82，5： | 59 |
| 2 | Re-Os geochronology of Cu and W-Mo deposits in the Balkhash metallogenic belt,Kazakhstan and its geological significance显示文摘<正>The Central Asian metallogenic domain(CAMD) is a multi-core metallogenic system controlled by boundary strike-slip fault systems.The Balkhash metallogenic belt in Kazakhstan,in which occur many large and super-large porphyritic Cu—Mo deposits and some quartz vein- and greisen-type W—Mo deposits,is a well-known porphyritic Cu—Mo metallogenic belt in the CAMD.In this paper 11 molybdenite samples from the western segment of the Balkhash metallogenic belt are selected for Re—Os compositional analyses and Re—Os isotopic dating.Molybdenites from the Borly porphyry Cu deposit and the three quartz vein-greisen W—Mo deposits—East Kounrad.Akshatau and Zhanet—all have relatively high Re contents(2712—2772μg/g for Borly and 2.267—31.50μg/g for the other three W—Mo deposits),and lower common Os contents(0.670—2.696 ng/g for Borly and 0.0051—0.056 ng/g for the other three).The molybdenites from the Borly porphyry Cu—Mo deposit and the East Kounrad,Zhanet,and Akshatau quartz vein- and greisen-type W—Mo deposits give average model Re—Os ages of 315.9 Ma,298.0 Ma,295.0 Ma,and 289.3 Ma respectively.Meanwhile,molybdenites from the East Kounrad,Zhanet,and Akshatau W—Mo deposits give a Re—Os isochron age of 297.9 Ma,with an MSWD value of 0.97.Re-Os dating of the molybdenites indicates that Cu—W—Mo metallogenesis in the western Balkhash metallogenic belt occurred during Late Carboniferous to Early Permian(315.9—289.3 Ma),while the porphyry Cu—Mo deposits formed at—316 Ma,and the quartz vein-greisen W—Mo deposits formed at ~298 Ma.The Re—Os model and isochron ages thus suggest that Late Carboniferous porphyry granitoid and pegmatite magmatism took place during the late Hercynian movement.Compared to the Junggar-East Tianshan porphyry Cu metallogenic belt in northwestern China,the formation of the Cu—Mo metallogenesis in the Balkhash metallogenic belt occurred between that of the Tuwu-Yandong in East Tianshan and the Baogutu porphyry Cu deposits in West Junggar. Collectively,the large-scale Late Carboniferous porphyry Cu—Mo metallogenesis in the Central Asian metallogenic domain is related to Hercynian tectono-magmatic activities. | Xuanhua Chen Wenjun Qu Shuqin Han Seitmuratova Eleonora Nong Yang Zhengle Chen Fagang Zeng Andao Du Zhihong Wang | 2010 | Geoscience Frontiers2010，1，1： | 10 |
| 3 | Dynamic Positioning System Based on Active Disturbance Rejection Technology显示文摘A dynamically positioned vessel, by the International Maritime Organization(IMO) and the certifying class societies(DNV, ABS, LR, etc.), is defined as a vessel that maintains its position and heading(fixed location or pre-determined track) exclusively by means of active thrusters. The development of control technology promotes the upgrading of dynamic positioning(DP) systems. Today there are two different DP systems solutions available on the market: DP system based on PID regulator and that based on model-based control. Both systems have limited disturbance rejection capability due to their design principle. In this paper, a new DP system solution is proposed based on Active Disturbance Rejection Control(ADRC) technology. This technology is composed of Tracking-Differentiator(TD), Extended State Observer(ESO) and Nonlinear Feedback Combination. On one hand, both TD and ESO can act as filters and can be used in place of conventional filters; on the other hand, the total disturbance of the system can be estimated and compensated by ESO, which therefore enhances the system's disturbance rejection capability. This technology's advantages over other methods lie in two aspects: 1) This method itself can not only achieve control objectives but also filter noisy measurements without other specialized filters; 2) This method offers a new useful approach to suppress the ocean disturbance. The simulation results demonstrate the effectiveness of the proposed method. | LEI Zhengling GUO Chen FAN Yunsheng | 2015 | Journal of Ocean University of China2015，14，4： | 3 |
| 4 | Dissipative particle dynamics simulation of gold nanoparticlesstabilization by PEO-PPO-PEO block copolymer micelles显示文摘 | Chen S Guo C Hu G H Liu H Z Liang X F Wang J Ma J H ZhengL | 2007 | Colloidand Polymer Science2007，285，14： | 1 |
| 5 | Influence of the ionic liquid 1- butyl-3-methylimidazolium chlorine on the ethanol fermentation of Saccharomyces cerevisiae AY93161 and its kinetics analysis 显示文摘 | ZhuSD YuP LeiMK TongYJ ZhengL ZhangR Ji J Chen Q M Wu Y X | 2013 | Energy Education Science and Technology Part A : Energy Science and Research2013，30，2： | 1 |
| 6 | A model for simulatingdeepwater oil and gas blowouts Part I : Theory and model for-mulation 显示文摘 | ZHENGL YAPA P D CHEN F H | 2002 | Journal of Hydraulic Research2002，41，4： | 1 |
| 7 | New evidence from stable isotope for the uplift of mountains in northern edge of the Qinghai-Tibetan Plateau显示文摘 | Zhengle Chen Xiaofeng Wang Xiahong Feng Changqiu Wang Jian Liu | 2002 | Science in China Series B: Chemistry2002，，1： | 1 |
| 8 | Chronological Constraints on Late Paleozoic Collision in the Southwest Tianshan Orogenic Belt, China: Evidence from the Baleigong Granites显示文摘The Baleigong granites, located in the western part of the southwestern Tianshan Orogen(Kokshanyan region, China), records late Paleozoic magmatism during the late stages of convergence between the Tarim Block and the Central Tianshan Arc Terrane. We performed a detailed geochronological and geochemical study of the Baleigong granites to better constrain the nature of collisional processes in the Southwest Tianshan Orogen. The LA-ICP-MS U-Pb zircon isotopic analyses indicate that magmatism commenced in the early Permian(~282 Ma). The granite samples, which are characterized by high contents of SiO2(67.68-69.77 wt%) and Al2O3(13.93-14.76 wt%), are alkali-rich and Mg-poor, corresponding to the high-K calc-alkaline series. The aluminum saturation index(A/CNK) ranges from 0.93 to 1.02, indicating a metaluminous to slightly peraluminous composition. Trace element geochemistry shows depletions in Nb, Ta, and Ti, a moderately negative Eu anomaly(δEu=0.40-0.56), enrichment in LREE, and depletion in HREE((La/Yb)N=7.46-11.78). These geochemical signatures are characteristic of an I-type granite generated from partial melting of a magmatic arc. The I-type nature of the Baleigong granites is also supported by the main mafic minerals being Fe-rich calcic hornblende and biotite. We suggest that the high-K, calc-alkaline I-type granitic magmatism was generated by partial melting of the continental crust, possibly triggered by underplating by basaltic magma. These conditions were likely achieved in a collisional tectonic setting, thus supporting the suggestion that closure of the South Tianshan Ocean was completed prior to the Permian and was followed(in the late Paleozoic) by collision between the Tarim Block and the Central Tianshan Arc Terrane. | HUO Hailong CHEN Zhengle ZHANG Qing HAN Fengbin ZHANG Wengao SUN Yue YANG Bin TANG Yanwen | 2019 | Acta Geologica Sinica(English Edition)2019，93，5： | 1 |
| 9 | New evidence from stable isotope for the uplift of mountains in northern edge of the Qinghai-Tibetan Plateau显示文摘 | Zhengle Chen Xiaofeng Wang Xiahong Feng Changqiu Wang Jian Liu | 2002 | Science in China Series B: Chemistry2002，，1： | 1 |
| 10 | MicroRNA155regulatesangiotensinII type 1 receptor expression and phenotypicdifferentiationinvascularadventitialfibroblasts显示文摘 | ZhengL Xu CC Chen WD etal | 2010 | BiochemBiophysResCommun2010，400，4： | 1 |
| 11 | Characteristics of Ore-forming Fluid of the Gaoshan Gold-Silver Deposit in the Longquan Area, Zhejiang Province and its Implications for the Ore Genesis显示文摘The Gaoshan gold-silver deposit, located between the Yuyao-Lishui Fault and JiangshanShaoxing fault in Longquan Area, occurs in the Suichang-Longquan gold-silver polymetallic metallogenic belt. This study conducted an investigation for ore-forming fluids using microthermometry, D-O isotope and trace element. The results show that two types of fluid inclusions involved into the formation of the deposit are pure liquid phase and gas-liquid phase aqueous inclusions. The homogenization temperature and salinity of major mineralization phase ranges from 156°C to 236°C(average 200°C) and 0.35% to 8.68%(NaCleqv)(average 3.68%), respectively, indicating that the ore-forming fluid is characteristic of low temperature and low salinity. The oreforming pressure ranges between in 118.02 to 232.13'105 pa, and it is estabmiated that the oreforming depth ranges from 0.39 to 0.77 km, indicating it is a hypabyssal deposit in genesis. The low rare earth elements content in pyrites, widely developed fluorite in late ore-forming stage and lack of chlorargyrite(Ag Cl), indicates that the ore-forming fluid is rich in F rather than Cl. The ratios of Y/Ho, Zr/Hf and Nb/Ta of between different samples have little difference, indicating that the later hydrothermal activities had no effects on the former hydrothermal fluid. The chondrite-normalized REE patterns of pyrites from country rocks and ore veins are basically identical, with the characteristics of light REE enrichment and negative Eu anomalies, implying that the ore-forming fluid was oxidative and derived partly from the country rocks. The δD and δ18O of fluid inclusions in quartz formed during the main metallogenic stage range from -105‰ to -69 ‰ and -6.01‰ to -3.81‰, respectively. The D-O isotopic diagram shows that the metallogenic fluid is characterized by the mixing of formation water and meteoric water, without involvement of magmatic water. The geological and geochemical characteristics of the Gaoshan gold-silver deposit are similar to those of continental volcanic hydrothermal deposit, and could be assigned to the continental volcanic hydrothermal gold-silver deposit type. | JIANG Biao WANG Chenghui CHEN Yuchuan WU Baogui LIAO Peng CHEN Zhengle HAN Fengbin | 2016 | Acta Geologica Sinica(English Edition)2016，90，4： | 0 |
| 12 | N^(6)-methyladenine is incorporated into mammalian genome by DNA polymerase显示文摘Dear Editor,DNA N^(6)-methylade nine(6mA),one of the most prevale nt epigenetic base modifications in prokaryotes,1 is recently found in multicellular eukaryotes.2-8 This nucleobase may have epigenetic roles in regulation of retrotransposons,chromatin organization,and so on.2-8 However,both our group9 and Greeks group10 noticed that eukaryotic DNA is easily contaminated with a minute of bacterial DNA,which carries overwhelmingly abundant 6mA(〜2%6mA/dA). | Xiaoling Liu Weiyi Lai Yao Li Shaokun Chen Baodong Liu Ning Zhang Jiezhen Mo Cong Lyu Jing ZhengL Ya-Rui Du Guibin Jiang Guo-Liang Xu Hailin Wang | 2021 | Cell Research2021，31，1： | 0 |
| 13 | Early Palaeozoic Granites in the Northern Tian Shan,Kyrgyzstan:Their Zircon Ages and Evolution Processes显示文摘The Tian Shan Orogenic Belt,which is a subsidiary of the Central Asian Orogenic Belt,is the largest accretion area of continental crust on the Earth during the Phanerozoic.It has experienced several accretionary processes during the Palaeozoic period and has attracted much concern among geologists.An Early Palaeozoic intrusive rock belt | XIAO Weifeng WANG Zongxiu CHEN Zhengle HAN Shuqin YU Xinqi | 2015 | Acta Geologica Sinica(English Edition)2015，89，3： | 0 |
| 14 | Metallogenesis and Geodynamic Setting of the Early Paleozoic Orogenic Gold Deposits in the North Altyn显示文摘The North Altyn has underwent a complex tectonic history in the Early Paleozoic and formed a number of orogenic gold deposits controlled by ductile to brittle shear zones adjacent to the southern side of the Northern Altyn Tagh fault e.g.the Dapinggou,Beiketan and Xiangyun.The Dapinggou gold deposit,a typical orogenic gold deposit in North Altyn,is predominantly hosted | WANG Yong CHEN Bailin CHEN Zhengle WU Yu | 2015 | Acta Geologica Sinica(English Edition)2015，89，3： | 0 |
| 15 | Structural Origin of the Red-Ribbon Style Iron Ores in the Xinyu Iron Deposit,Central Jiangxi Province显示文摘In summary,field observations and detailed measurements suggest that the red-ribbon style iron-ore bodies in Xinyu iron deposit result from regional plastic flow and sausage bending,rather than fold superimposition.The Xinyu iron deposit,located in central Jiangxi Province,is one of the most important BIF-type deposits in China.It is hosted in the Late Proterozoic volcanicsedimentary rocks,which are composed of sericitechlorite pyhllite,magnetite-bearing chlorite phyllite or schist,magnetite quartzite,and schist(Yu et al.,1989;Zeng et al.,2011).The Xinyu iron orefield lies on the eastern side of the Wugong Shan uplift,to the north of the South | CHEN Zhengle ZHANG Qing CHEN Bailin WANG Xueping SHEN Tao WU Junjie | 2015 | Acta Geologica Sinica(English Edition)2015，89，2： | 0 |
| 16 | New Ar-Ar Isotopic Ages of the Southern Tianshan Mountains, Kyrgyzstan and their Geological Implications显示文摘Objective The Late Paleozoic Southern Tianshan Ocean is usually considered to be the last-closed ocean in the Tianshan Orogeny.However,there is still no consensus if this is indeed the case.Blueschist,eclogite and ophiolite are present in the Atbashi Range,Kyrgyzstan,which are believed to be the relics of the Southern Tianshan Ocean.New data obtained through Ar-Ar isotopic analysis in | XIAO Weifeng WANG Zongxiu CHEN Zhengle HAN Shuqin YU Xinqi | 2018 | Acta Geologica Sinica(English Edition)2018，92，4： | 0 |
| 17 | Elephant Culture Matter for China’s Asian Elephants Conservation显示文摘Traditional anthropogenic impacts such as hunting,using as war-elephant,trading of ivory,paying tribute to the imperial court and so on,were once thought to be directly responsible for the rapid decline of Asian elephants in China.But in Yunnan Province,China,a unique human factor such as the traditional elephant culture of local ethnic minorities,is an important factor in the conservation of Asian elephants.In these areas,we investigated by means of village interviews,field surveys and data collection,the results show that the elephant culture of ethnic minorities has a great impact on people’s thoughts and behaviors,these traditional culture and belief(that mean taking elephant as the God,holding elephant as a belief,worshipping elephant and praise it)urges people to actively protect elephants and avoid more human-elephant conflicts.To enhance the public awareness of Asian elephant conservation,the Chinese Government or international environmental organizations should give higher attention and support to these elephant cultures. | Yongjing Tang Zhengling Li Guilian Jiang Ting Lv Lei Zhang Wenlan Zhao Gaofan Zhu Mingyong Chen | 2020 | Journal of Zoological Research2020，2，2： | 0 |
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