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| 1 | Exogenous plant MIR168a specifically targets mammalian LDLRAPI: evidence of cross-kingdom regulation by microRNA显示文摘 | Lin Zhang Dongxia Hou Xi Chen Donghai Li Lingyun Zhu Yuj ing Zhang Jing Li Zhen Bian Xiangying Liang Xing Cai Yuan Yin Cheng Wang Tianfu Zhang Dihan Zhu Dianmu Zhang Jie Xu Qun Chen Yi Ba Jing Liu Qiang Wang Jianqun Chen Jin Wang Meng Wang Qipeng Zhang Junfeng Zhang Ke Zen Chen-Yu Zhang | 2012 | Cell Research2012,22,1: | 155 |
| 2 | GL3.3, a Novel QTL Encoding a GSK3/SHAGGY- like Kinase, Epistatically Interacts with GS3 to Produce Extra-long Grains in Rice显示文摘 | Duo Xia Nao Zhou Rongjia Liu Wenhan Dan Pingbo Li Bian Wu Junxiao Chen Lingqiang Wang Guanjun Gao Qinglu Zhang Yuqing He | 2018 | Molecular Plant2018,11,5: | 41 |
| 3 | Pathological evidence for residual SARS-CoV-2 in pulmonary tissues of a ready-for-discharge patient显示文摘Dear Editor,SARS-CoV-2,a novel coronavirus and causing COVID-19,has given rise to a worldwide pandemic.1,2 So far,tens of thousands of COVID-19 patients have been clinically cured and discharged,but multiple COVID-19 cases showed SARS-CoV-2 positive again in discharged patients,3 which raises an attention for the discharged patients.Also,there is an urgent need to understand the pathogenesis of SARS-CoV-2 infection.Here,we conducted postmortem pathologic study in a ready-fordischarge COVID-19 patient who succumbed to sudden cardiovascular accident.Pathological examination revealed SARSCoV-2-viruses remaining in pneumocytes and virus-caused pathological changes in the lungs.Our study provided new insights into SARS-CoV-2 pathogenesis and might facilitate the improvement of clinical guideline for virus containment and disease management. | Xiao-Hong Yao Zhi-Cheng He Ting-Yuan Li Hua-Rong Zhang Yan Wang Huaming Mou Qiaonan Guo Shi-Cang Yu Yanqing Ding Xindong Liu Yi-Fang Ping Xiu-Wu Bian | 2020 | Cell Research2020,30,6: | 35 |
| 4 | AXL is a candidate receptor for SARS-CoV-2 that promotes infection of pulmonary and bronchial epithelial cells显示文摘The current coronavirus disease 2019(COVID-19)pandemic presents a global public health challenge.The viral pathogen responsible,severe acute respiratory syndrome coronavirus 2(SARS-CoV-2),binds to the host receptor ACE2 through its spike(S)glycoprotein,which mediates membrane fusion and viral entry.Although the role of ACE2 as a receptor for SARS-CoV-2 is clear,studies have shown that ACE2 expression is extremely low in various human tissues,especially in the respiratory tract.Thus,other host receptors and/or co-receptors that promote the entry of SARS-CoV-2 into cells of the respiratory system may exist.In this study,we found that the tyrosine-protein kinase receptor UFO(AXL)specifically interacts with the N-terminal domain of SARS-CoV-2 S.Using both a SARS-CoV-2 virus pseudotype and authentic SARS-CoV-2,we found that overexpression of AXL in HEK293T cells promotes SARS-CoV-2 entry as efficiently as overexpression of ACE2,while knocking out AXL significantly reduces SARS-CoV-2 infection in HI 299 pulmonary cells and in human primary lung epithelial cells.Soluble human recombinant AXL blocks SARS-CoV-2 infection in cells expressing high levels of AXL.The AXL expression level is well correlated with SARS-CoV-2 S level in bronchoalveolar lavage fluid cells from COVID-19 patients.Taken together,our findings suggest that AXL is a novel candidate receptor for SARS-CoV-2 which may play an important role in promoting viral infection of the human respiratory system and indicate that it is a potential target for future clinical intervention strategies. | Shuai Wang Zongyang Qiu Yingnan Hou Xiya Deng Wei Xu Tingting Zheng Peihan Wu Shaofang Xie Weixiang Bian Chong Zhang Zewei Sun Kunpeng Liu Chao Shan Aifu Lin Shibo Jiang Youhua Xie Qiang Zhou Lu Lu Jing Huang Xu Li | 2021 | Cell Research2021,31,2: | 39 |
| 5 | A Positioning System based on Communication Satellites and the Chinese Area Positioning System(CAPS)显示文摘The Chinese Area Positioning System(CAPS) is a positioning system based on satellite communication that is fundamentally different from the 3'G'(GPS,GLONASS and GALILEO) systems.The latter use special-purpose navigation satellites to broadcast navi-gation information generated on-board to users,while the CAPS transfers ground-generated navigation information to users via the communication satellite.In order to achieve accurate Positioning,Velocity and Time(PVT),the CAPS employs the following strategies to over-come the three main obstacles caused by using the communication satellite:(a) by real-time following-up frequency stabilization to achieve stable frequency;(b) by using a single carrier in the transponder with 36 MHz band-width to gain sufficient power;(c) by incorporating Decommissioned Geostationary Orbit communication satellite(DGEO),barometric pressure and Inclined Geostationary Orbit communication satellite(IGSO) to achieve the 3-D posi-tioning.Furthermore,the abundant transponders available on DGEO can be used to realize the large capacity of communication as well as the integrated navigation and communication.With the communication functions incorporated,five new functions appear in the CAPS:(1) combination of navigation and communication;(2) combination of navigation and high accu-racy orbit measurement;(3) combination of navigation message and wide/local area differen-tial processing;(4) combination of the switching of satellites,frequencies and codes;and(5) combination of the navigation message and the barometric altimetry.The CAPS is thereby labelled a PVT5C system of high accuracy.In order to validate the working principle and the performance of the CAPS,a trial system was established in the course of two years at a cost of about 20 million dollars.The trial constellation consists of two GEO satellites located at E87.5° and E110.5°,two DGEOs located at E130° and E142°,as well as barometric altimetry as a virtual satellite.Static and dynamic performance tests were completed for the Eastern,the Western,the Northern,the Southern and the Middle regions of China.The evaluation results are as follows:(1) land static test,plane accuracy range:C/A code,15~25m;P code,5~10 meters;altitude accuracy range,1~3 m;(2) land dynamic test,plane accuracy range,C/A code,15~25m;P code,8~10m;(3) velocity accuracy,C/A code,0.13~0.3ms-1,P code,0.15~0.17ms-1;(4) timing accuracy,C/A code,160ns,P code,13 ns;(5) timing compared accuracy of Two Way Satellite Time and Frequency Transfer(TWSTFT),average accuracy,0.068ns;(6) random error of the satellite ranging,10.7 mm;(7) orbit determination accuracy,better than 2 m.The above stated random error is 1σ error.At present,this system is used as a preliminary operational system and a complete system with 3 GEO,3 DGEO and 3 IGSO is being established. | Guo-Xiang Ai Hu-Li Shi Hai-Tao Wu Yi-Hua Yan Yu-Jing Bian Yong-Hui Hu Zhi-Gang Li Ji Guo Xian-De Cai | 2008 | Chinese Journal of Astronomy and Astrophysics2008,8,6: | 33 |
| 6 | Outbreak of Dengue Fever in Central China,2013显示文摘In 2013,the first dengue fever(DF) outbreak in central China was reported in the central of Henan province,northern temperate regions,although they have been sequentially recorded in Southern China.106 suspected DF cases were reported and 73 patients were confirmed dengue virus type 3(DEN-3) infections.62/392(15.8%) local health persons showed DEN antibodies positive.To this day Henan is the northernmost province in China which has been reported about outbreak of DF and what is important is that it warns us the endemic range of DF has been expanded geographically in China. | HUANG Xue Yong MA Hong Xia WANG Hai Feng DU Yan Hua SU Jia LI Xing Le TANG Xiao Yan MA Hong Peng ZU Bing Can ZHANG Qiao Hong CHEN Hao Min XU Bian Li | 2014 | Biomedical and Environmental Sciences2014,27,11: | 30 |
| 7 | Efficacy and safety of Xiangsha Liujunzi granules for functional dyspepsia: A multi-center randomized double-blind placebo-controlled clinical study显示文摘AIM To assess the efficacy and safety of a Chinese herbal medicine(CHM), Xiangsha Liujunzi granules, in the treatment of patients with functional dyspepsia(FD). METHODS We performed a randomized, double-blind, placebocontrolled trial with patients from three centers. Two hundred and sixteen subjects diagnosed with FD according to ROME Ⅲ criteria and confirmed by upper gastrointestinal endoscopy and spleen-deficiency and Qi-stagnation syndrome were selected to receive Xiangsha Liujunzi granules or placebo for 4 wk in a 2:1 ratio by blocked randomization. The subjects also received follow-up after the 4-wk intervention. Herbal or placebo granules were dissolved in 300 m L of water. Participants in both groups were administered 130 m L(45 ℃) three times a day. Participants were evaluated prior to and following 4 wk of the intervention in terms of changes in the postprandial discomfort severity scale(PDSS) score, clinical global impression(CGI) scale score, hospital anxiety and depression scale(HADS) score, traditional Chinese medicine symptoms score(SS), scores of various domains of the 36-item short form health survey(SF-36), gastric emptying(GE) and any observed adverse effects. RESULTS Compared with the placebo group, patients in the CHM group showed significant improvements in the scores of PDSS, HADS, SS, SF-36 and CGI scale(P < 0.05 or P < 0.01). They also showed the amelioration in the GE rates of the proximal stomach and distal stomach(P < 0.05 or P < 0.01).CONCLUSION Xiangsha Liujunzi granules offered significant symptomatic improvement in patients with FD. | Lin Lv Feng-Yun Wang Xiang-Xue Ma Zhen-Hua Li Sui-Ping Huang Zhao-Hong Shi Hai-Jie Ji Li-Qun Bian Bei-Hua Zhang Ting Chen Xiao-Lan Yin Xu-Dong Tang | 2017 | World Journal of Gastroenterology2017,23,30: | 29 |
| 8 | Preliminary Scientific Results of Chang'E-1 Lunar Orbiter:Based on Payloads Detection Data in the First Phase显示文摘Chang'E-1 lunar Orbiter was launched by Long March 3A rocket from Xichang Satel-lite Launch Center at 18:05BT(Beijing Time) Oct.24,2007.It is the first step of its ambitious three-stage moon program,a new milestone in the Chinese space exploration history.The primary science objectives of Chang'E-1 lunar orbiter are to obtain three-Dimension(3D) stereo images of the lunar surface,to analyze the distribution and abundance of elements on the surface,to investigate the thickness of lunar soil,evaluate helium-3 resources and other characteristics,and to detect the space environment around the moon.To achieve the above four mission objectives,eight sets of scientific instruments are chosen as the payloads of the lunar orbiter,including a CCD stereo camera(CCD),a Sagnac-based interferometer spectrometer(ⅡM),a Laser Altimeter(LAM),a Microwave Radiometer(MRM),a Gamma-Ray Spectrometer(GRS),an X-ray spectrometer(XRS),a High-Energy Particle Detector(HPD),and two Solar Wind Ion Detectors(SWID).The detected data of the payloads show that all payloads work well.This paper introduces the status of payloads in the first phase and preliminary scientific results. | OUYANG Ziyuan JIANG Jingshan LI Chunlai SUN Huixian ZOU Yongliao LIU Jianzhong LIU Jianjun ZHAO Baochang REN Xin YANG Jianfeng ZHANG Wenxi WANG Jianyu MOU Lingli CHANG Jin ZHANG Liyan WANG Huanyu LI Yongquan ZHANG Xiaohui ZHENG Yongchun WANG Shijin BIAN Wei | 2008 | 空间科学学报2008,28,5: | 24 |
| 9 | The global image of the Moon obtained by the Chang'E-1:Data processing and lunar cartography显示文摘The global lunar image of the first phase of Chinese Lunar Exploration Program is the first image that covered all over the surface of the Moon. It will serve as a critical foundation for succeeding exploration and scientific research. In this paper, the acquisition, characteristics, and data quality of Chang'E-1 CCD image data are described in detail. Also described are the methodology and procedure of data processing. According to rule of planetary cartography, the image data have been processed, geometrically corrected, and then mosaicked and merged in a scale of 1:2.5 million. The results of data processing and charting show that the image data of Chang'E-1 CCD and their geometric precision meet the demand of charting a map in the scale of 1:2.5 million. The relative geometric positioning precision of the global image is better than 240 m, and the absolute geometric positioning precision is slightly better than that of the ULCN2005 and Clementine lunar basemap (V2.0). The plane positioning precision is approximately 100-1500 m. This global image proves to be the best global image of the Moon so far in terms of space coverage, image quality, and positioning precision. | LI ChunLai1, LIU JianJun1, REN Xin1, MOU LingLi1, ZOU YongLiao1, ZHANG HongBo1, Lü Chang1, LIU JianZhong1, ZUO Wei1, SU Yan1, WEN WeiBin1, BIAN Wei1, ZHAO BaoChang2, YANG JianFeng2, ZOU XiaoDuan1, WANG Min1, XU Chun1, KONG DeQing1, WANG XiaoQian1, WANG Fang1, GENG Liang1, ZHANG ZhouBin1, ZHENG Lei1, ZHU XinYing1, LI JunDuo1 & OUYANG ZiYuan11 National Astronomical Observatories, Chinese Academy of Sciences, Beijing 100012, China 2 Xi’an Institute of Optics and Precision Mechanics, Chinese Academy of Sciences, Xi’an 710119, China | 2010 | Science China Earth Sciences2010,53,8: | 22 |
| 10 | Preliminary evidence indicating Dome A (Antarctica) satisfying preconditions for drilling the oldest ice core显示文摘Lowest temperature and snow accumulation rate are preconditions for retrieving the oldest ice core from the polar ice sheets. The 10-m depth firn temperature at Dome A, the summit of the Antarctic Ice Sheet, recorded by an automatic weather station (AWS) was -58.3℃ in 2005 and -58.2℃ in 2006, re-spectively. The 10-m firn temperature is an approximation of the annual mean air temperature (AMAT), and this is the lowest AMAT that has been recorded on the surface of the Earth. The stable isotopic ratios (δ 18O and δ D) of surface snow at Dome A are also lower than at other ice sheet domes along the East Antarctic Ice Divide such as Dome C, Dome F, Dome B and Vostok. These facts indicate that Dome A is the 'pole of cold' on the Earth. The total amount of snow accumulation rate in 2005 and 2006 was only 0.16 cm, equaling 0.016 m water equivalent per year, the lowest precipitation ever recorded from Antarctica. Preliminary evidences indicate that Dome A is a candidate site for recovering the oldest ice core. | XIAO CunDe LI YuanSheng HOU ShuGui lan ALLISON BIAN LinGen REN JiaWen | 2008 | Chinese Science Bulletin2008,53,1: | 23 |
| 11 | The discovery of Palaeoproterozoic volcanic rocks in the Bulunkuoler Group from the Tianshuihai Massif in Xinjiang of Northwest China and its geological significance显示文摘In the Dabudaer region of the Tianshuihai Massif (Xinjiang, Northwest China), metavolcanic rocks within the mainly meta-sedimentary Bulunkuoler Group are basalt, basaltic andesite, and rhyolite. In situ zircon U-Pb LA-ICP-MS dating on rhyolite magmatic zircons yielded an age of 2481±14 Ma, interpreted as the eruption age of the Bulunkuoler Group volcanic rocks. The basalt and basaltic andesite are low-Al tholeiite series and the rhyolite is low-Al calc-alkaline series. All of rocks are charac-terized by enrichment of LREE and LILE (Rb, Th and Ba), depletion of P, Nb, Ta and Ti, and absence of Eu anomalies. The εNd(t) of basalts ranges from 3.14 to 4.88 indicating a depleted mantle source. The trace element signatures show that these magmas experienced intense crustal contamination during their ascent. Direct evidence for crustal contamination is the xenocrystic zircons in the ryholite, with ages back to ca. 3300 Ma. The primitive-mantle normalized and Zr/Y-Zr diagrams for the basic volcanic rocks show that they formed in an intra-continental tectonic setting. Combined with the previous studies and compared with North China Craton Neoarchean basic volcanic rocks, it is supposed that the Bulunkuoler Group volcanic rocks reflect the Palaeoproterozoic mantle magma underplating and interaction with felsic crust. | JI WenHua LI RongShe CHEN ShouJian HE ShiPing ZHAO ZhenMing BIAN XiaoWei ZHU HaiPing CUI JiGang REN JuanGang | 2011 | Science China Earth Sciences2011,54,1: | 22 |
| 12 | Liguzinediol improved the heart function and inhibited myocardial cell apoptosis in rats with heart failure显示文摘 | Yu LI Ping SONG Qing ZHU Qiu-yi YIN Jia-wen JI Wei LI Hui-min BIAN | 2014 | Acta Pharmacologica Sinica2014,35,10: | 23 |
| 13 | The second natural gas hydrate production test in the South China Sea显示文摘Clayey silt reservoirs bearing natural gas hydrates(NGH)are considered to be the hydrate-bearing reservoirs that boast the highest reserves but tend to be the most difficult to exploit.They are proved to be exploitable by the first NGH production test conducted in the South China Sea in 2017.Based on the understanding of the first production test,the China Geological Survey determined the optimal target NGH reservoirs for production test and conducted a detailed assessment,numerical and experimental simulation,and onshore testing of the reservoirs.After that,it conducted the second offshore NGH production test in 1225 m deep Shenhu Area,South China Sea(also referred to as the second production test)from October 2019 to April 2020.During the second production test,a series of technical challenges of drilling horizontal wells in shallow soft strata in deep sea were met,including wellhead stability,directional drilling of a horizontal well,reservoir stimulation and sand control,and accurate depressurization.As a result,30 days of continuous gas production was achieved,with a cumulative gas production of 86.14×104 m3.Thus,the average daily gas production is 2.87×10^4 m^3,which is 5.57 times as much as that obtained in the first production test.Therefore,both the cumulative gas production and the daily gas production were highly improved compared to the first production test.As indicated by the monitoring results of the second production test,there was no anomaly in methane content in the seafloor,seawater,and atmosphere throughout the whole production test.This successful production test further indicates that safe and effective NGH exploitation is feasible in clayey silt NGH reservoirs.The industrialization of hydrates consists of five stages in general,namely theoretical research and simulation experiments,exploratory production test,experimental production test,productive production test,and commercial production.The second production test serves as an important step from the exploratory production test to experimental production test. | Jian-liang Ye Xu-wen Qin Wen-wei Xie Hai-long Lu Bao-jin Ma Hai-jun Qiu Jin-qiang Liang Jing-an Lu Zeng-gui Kuang Cheng Lu Qian-yong Liang Shi-peng Wei Yan-jiang Yu Chunsheng Liu Bin Li Kai-xiang Shen Hao-xian Shi Qiu-ping Lu Jing Li Bei-bei Kou Gang Song Bo Li He-en Zhang Hong-feng Lu Chao Ma Yi-fei Dong Hang Bian | 2020 | China Geology2020,3,2: | 22 |
| 14 | Molecular network-based analysis of Guizhi- Shaoyao-Zhimu decoction, a TCM herbal formula, for treatment of diabetic peripheral neuropathy显示文摘目的: Guizhi-Shaoyao-Zhimu 煎(GSZ ) ,繁体中文药(TCM ) 草药的公式,被显示出在糖尿病的外部神经病(DPN ) 的治疗有效。在这研究,网络分析被执行译解在 DPN 的处理的 GSZ 的分子的机制。 | Ning ZHAO Jian LI Li LI Xu-yan NIU Miao JIANG Xiao-juan HE Zhao-xiang BIAN Ge ZHANG Ai-ping LU | 2015 | Acta Pharmacologica Sinica2015,36,6: | 21 |
| 15 | Comparative study of gas accumulations in the Permian Changxing reefs and Triassic Feixianguan oolitic reservoirs between Longgang and Luojiazhai-Puguang in the Sichuan Basin显示文摘Reef and oolitic gas reservoirs in the Permian Changxing and Triassic Feixianguan formations have been discovered in both the Luojiazhai-Puguang and Longgang areas of the Sichuan Basin, but the accumulation scale, abundance and distribution patterns differ greatly. In fact, the two areas have more differences than they have similarities. Similarities include: (1) the lithology, properties and types of porosity of the reef and oolitic reservoirs are primarily consistent in the two areas; (2) well-developed regional caprocks that seal the fluid system; and (3) accumulation process histories, with liquid hydrocarbon charging at an early stage, cracking into gas at a high to over-mature stage, adjustment of gas reservoirs at an uplifting stage, and final reservoir generation at a late stage. Differences include: (1) gas accumulations in the Luojiazhai-Puguang area that are dominated by oil-type cracked gas, with multiple and sufficient gas sources, contrasting with gas accumulations in the Longgang area that are dominated by coal-sourced gas with insufficient gas sources; (2) heterogeneity and horizontal diversity of reservoirs in the Longgang area that are stronger than in the Luojiazhai-Puguang area; and (3) the development of deep and large faults in the Luojiazhai-Puguang area that link source, reservoir and migration pathways, contrasting with poorly developed faults in Longgang area, where laterally variable fractures are the major migration pathway. Because of these differences, abundant large-scale structurally-controlled gas accumulations are developed in the Luojiazhai-Puguang area, whereas lithology plays a more important role in gas accumulation in the Longgang area where accumulations are smaller-scale and have lower gas-bearing abundance. We suggest that future exploration for reef and oolitic gas accumulations should be strengthened in NE Sichuan and NW Sichuan Jiulongshan. In particular, the transitional zone between Longgang and Kaijiang-Liangping Bay has the best potential for new discoveries. | ZHAO WenZhi XU ChunChun WANG TongShan WANG HongJun WANG ZeCheng BIAN CongSheng LI Xia | 2011 | Chinese Science Bulletin2011,56,31: | 21 |
| 16 | Research Progress in Occupational Health Risk Assessment Methods in China显示文摘Traditional occupational disease control and prevention has remained prevalent in China over recent decades.There are appropriately 30,000 new case reports of occupational diseases annually.Although China has already established a series of occupational disease prevention programs,occupational health risk assessment(OHRA)strategies continue to be a limitation.OHRA is a tool for controlling the health | ZHOU Li Fang TIAN Fang ZOU Hua YUAN Wei Ming HAO Mo ZHANG Mei Bian | 2017 | Biomedical and Environmental Sciences2017,30,8: | 20 |
| 17 | A Study of the Kunlun-Qilian-Qinling Suture System显示文摘The Late Neoproterozoic-Early Palaeozoic suture zones within theCentral Orogenic Belt of China can be considered a system-the Kunlun-Qilian-Qinling suture system (KQQ suture system). It is basically divided into the western, central and eastern sectors. The western sector consists of the Küda-Subashi suture zone, the Mazar Kangxiwar suture and the central West Kunlun microblock. The central sector covers the following five suture zones: the Altun, North Qilian, Qaidam northern marginal, Qimantag-Wutuo and East Kunlun southern marginal sutures, in addition to some microblocks such as the mid-south Qilian, Qaidam, Ayakkum and Maqen microblocks. The eastern sector is composed of the Shangdan suture zone, Mianlüe suture zone and central Qinling-Dabie microblock. The KQQ suture system experienced (1) extending-rifting of the Rodinia super-continent in the early-middle Sinian (~780-600 Ma); (2) the formation and evolution of the KQQ archipelagic ocean during the Late Sinian-Ordovician (~600-440 Ma), and (3) closing of the KQQ ocean and forming of the KQQ suture system during the Late Ordovician-early Silurian (~440-400 Ma). As a system comprising many suture zones and microblocks, the KQQ suture system consti tutes the foundation of the Central Orogenic Belt of China.CLC Number:P5 Document ID:Afoundation Item:This study was supported by the National Natural Science Foundation of China (grants 49872077 and 49572153), and the Lu Jiaxi Foundation of the Chinese Academy of Sciences.Author Resume:Bian Qiantao Born in 1945; graduated from the Department of Geology, South-Central University of Technology in 1970, and obtained his master's degree and doctor's degree at the Graduate School and the Institute of Geology, Chinese Academy of Sciences in 1981 and 1987, respectively. He is currently a professor of the Institute of Geology and Geophysics, Chinese Academy of Sciences, and has long been engaged in the research of tectonics, petrology, mineral deposits and geochemistry. Tel: (010) 62008058: E-mail:bianqt @igcas.igcas.ac.cn. References:[1]Integrated Scientific Expedition to the Qinghai-Xizang Plateau, Chinese Academy of Sciences, 2000. Geological Evolution of the Karakorum and Kunlun Mountains. Beijing: Science Press, 393-513 (in Chinese).[2]Bian Qiantao, Lin Chuanyong and Shi Lanbin, 1995. Microstruracmral features of metaperidotites in Küda, Western Kunlun, China. Scientia Geologica Sinica, 30 (3): 275-282 (in Chinese with English abstract).[3]Bian Qiantao, Chang Chengfa and Zheng Xianshen, 1997. Basic geotectonic characteristics of the Hoh Xil region of Qinghai Province, China. Scientia Geologica Sinica, 32(1): 37-46 (in Chinese with English abstract).[4]Bian Qiantao, Luo Xiaoquan, Li Dihui et al., 1999a. Zircon U-Pb age of granodiorite-tonalite in the Anyemaqen ophiolitic belt and its tectonic significance. Scientica Geologica Sinica, 34 (4): 420-426 (in Chinese with English abstract).[5]Bian Qiantao, Luo Xiaoquan, Li Hongsheng et al., 1999b. Discovery of Early Palaeozoic and Early Carboniferous-Early Permian ophiolites in the A'nyemaqen Mrs., Qinghai Province, China. Scientia Geologica Sinica (English edition), 8(3): 437-438.[6]Bian Qiantao, Yin Leiming, Sun Shufen et al., 200la. Discovery of Ordovician acritarchs in Buqingshan ophiolite mélange, East Kunlun Mountains, and its significance. Chinese Science Bulletin (English edition), 46(4): 341-345.[7]Bian Qiantao, Luo Xiaoquan, Li Dihui, Zhao Dasheng et al., 200lb. Geochemistry and formation environment of the Buqingshan ophiolite mélange, Qinghai Province, China. Acta Geologica Sinica, 75 (1): 45-55 (in Chinese with English abstract).[8]Cao Yongqing, Luo Zhaohua, Deng Jinfu et al., 1999. Palaeozoic volcanic activities and tectonic evolution of the Eastern Kunlun Mountains - the northern margin of the Qaidam Basin. Geological Review, 45 (supplement): 1002-1009 (in Chinese with English abstract).[9]Cheng Guoliang, Sun Yuhang, Sun Qingge et al., 1995. Palaeomagnetic research on the Phanerozoic tectonic evolution of China. Seismology and Geology, 17(1): 69-78 (in Chinese with English abstract).[10]Cui Junwen, Tang Zhemin, Deng Jinfu et al., 1999. Altun Fault System Beijing: Geological Publishing House, 95-97 (in Chinese with English abstract).[11]Cui Zhilin, Sun Yong and Wang Xueren, 1996. A discovery of Radiolaria from Danfeng ophiolites, North Qinling and its tectonic significance. Chinese Science Bulletin (English edition), 41(11): 916-919.[12]Cui Zhilin, Hua Hong and Song Qingyuan, 2000. The Late Ordovician radiolaria assemblage of the North Qinling back arc basin, China. Acta Geologica Sinica (English edition), 74 (3): 254-258.[13]Dalziel, I.W.D., 1997. Neoproterozoic-Palaeozoic geography and tectonics: reviews, hypothesis, and environmental speculation. Geol. Soc. Am Bull., 109(1): 16-42.[14]Deng Wanming. 1995. Geological feature of ophiolite and tectonic significance in the Karakorum-West Kunlun Mts. Acta Petrologica Sinica, 1l(Suppl.): 98-111 (in Chinese with English abstract).[15]Ding Daogui, Tang Liangjie et al., 1996. Formation and Evolution of the Tarim Basin. Nanjing: Hehai University Press, 302 (in Chinese with English abstract).[16]Du Yuansheng, Yin Hongfu and Wang Zhiping, 1997. The late Caledonian-early Hercynian basin's framework and tectonic evolution of Qinling orogenic belt. Earth Science, 22(4): 401-405 (in Chinese with English abstract).[17]Feng Yimin and He Shiping, 1995. Research for geology and geochemistry of several ophiolites in the North Qilian Mountains, China. Acta Petrologica Sinica, 1l(suppl.): 125-146 (in Chinese with English abstract).[18]Feng Yimin and He Shiping, 1996. Geotectonics and Orogeny of the Qilian Mountains, China. Beijing: Geological Publishing House, 135 (in Chinese with English abstract).[19]Hoffman, P.F., 1991. Did the breakout of Laurentia turn Gondwanaland inside-out? Science, 252:1406-1412.[20]Huang, B.C., Yang, Z.Y., Otofuji, Y-I., and Zhu, R.X., 1999. Early Palaeozoic palaeomagnetic poles from the western part of the North China Block and their implications. Tectonophysics, 308: 377-402.[21]Jiang Chunfa, Yang Jingshui, Feng Binggui et al., 1992. Opening Closing Tectonics of Kunlun Mountains. Beijing: Geological Publishing House, 135-171 (in Chinese with English abstract).[22]Jiang Chunfa, Wang Zhongqi and Li Jinyi, 2000. Opening Closing Tectonics of the Central Orogenic Belt in China. Beijing: Geological Publishing House, 135-171 (in Chinese with English abstract).[23]Lai Shaocong, Deng Jinfu and Zhao Hailing, 1996. Palaeozoic ophiolites and its tectonic significance on north margin of Qaidam Basin. Geoscience, 10 (1): 18-28 (in Chinese with English abstract).[24]Lai Shaocong and Zhang Guowei, 1999. Ophiolites and their tectonic significance in the Mianlüe suture zone, Qinling Dabie orogenic belt. Geological Review, 45(sup.): 1062-1071 (in Chinese with English abstract).[25]Li Shuguang, Sun Weidong, Zhang Guowei et al., 1996. Chronology and geochemistry of metavolcanic rocks from Heigouxia Valley in the Mianlüe tectonic zone, South Qinling: evidence for a Palaeozoic oceanic basin and its closure time. Science in China (Series D) (English edition), 39(3): 300-310.[26]Li Yaseng, Cao Xuanzuo, Yang Jialu et al., 1994. Sedimentation and Evolution of the Qinling Ancient Ocean Basin in Phanerozoic Eon. Beijing: Geological Publishing House, 166-183 (in Chinese).[27]Li, Z.X., Zhang, L, and Powell C.McA., 1996. Positions of the East Asian cratons in the Neoproterozoic supercontinent Rodinia. Australian Journal of Earth Sciences, 43: 591-592.[28]Liu Liang, Che Zicheng, Wang Yan et al., 1998. The evidence of Sm-Nd isochron age for the early Palaeozoic ophiolite in Mangya area, Altun Mountains. Chinese Science Bulletin (English edition), 43(9): 754-756.[29]Liu Liang, 1999. High-pressure metamorphic rock and ophiolite and their tectonic significance in Altun Mountains. Ph.D paper, the Institute of Geology, Chinese Academy of Sciences.[30]Lu Songnian, 1998. A review of advance in the research on the Neoproterozoic Rodinia Supercontinent. Geological Review, 44(5): 489-495 (in Chinese with English abstract).[31]Meng Qingren and Zhang Gouwei, 1999. Timing of collision of the North and South China blocks: controversy and reconciliation. Geology, 27(2): 123-126.[32]Pan Yusheng, Zhou Weiming, Xu Ronghua, Wang Dong'an, Zhang Yuquan, Xie Yingwen, Chen Tingen and Luo Hui, 1996. Geological characteristics and elolution of the Kunlun Mountain region during the early Paleozoic. Science in China (Series D) (English edition), 39(4): 337-347.[33]Scotese, C.R., McKerrow, W.S., 1990. Revised world maps and introduction. Geol. Soc. London Mem. 12: 1-21.[34]Song Shuguang, 1997. Tectonic evolutin of subductive complex belts in the North Qilian Mountains. Advance in Earth Sciences, 12(4): 351-365 (in Chinese with English abstract).[35]Wang Dong'an, Chen Ruijun, 1989. Petrological characteristics and depositional environment of the pelaegic ophiolitic sedimentrary rocks of Yixiekegou on the northwest of Kudi, Xinjiang. Journal of Natural Resources, 4 (3): 212-221(in Chinese with English abstract).[36]Wang Jianghai, 1998. New advances in reconstruction of the Proterozoic Rodinia Supercontinent. Earth Science Frontiers, 5(4): 235-242 (in Chinese with English abstract).[37]Wang Yan, Liu Liang, Che Zicheng et al., 1999. Geochemical characteristics of early Palaeozoic ophiolite in Mangnai area, Altun Mountains. Geological Review, 45(sup.): 1010-1014 (in Chinese with English abstract).[38]Wen Daren and Smith, A., 2000. Neoproterozoic-Early Palaeozoic tectonic evolution of the Qilian Orogenic Belt and its correlations with Gondwana. Abstracts of the Second Cross-Strait Conference on Geology of the Qilian Mountains and Adjacent Areas, 148-152.[39]Wu Jieren, Ren Bingshen, Zhang Mei et al., 1987. The genetic type and geological characteristics of the Xitieshan massive sulphide deposit, Qinghai Province. Bulletin of the Xi'an Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 20:1-81 (in Chinese with English abstract).[40]Xia Linqi, Xia Zuchun and Xu Xueyi, 1996. Genesis of Marine Volcanic Rocks in North Qilian Mountains. Beijing: Geological Publishing House, 153 (in Chinese).[41]Xia Linqi, Xia Zuchun, Xu Xueyi et al., 1999. Proterozoic continental flood basalts from Qilian Mountains. Geological Review, 45(sup.): 1028-1037 (in Chinese with English abstract).[42]Xia Lingqi, Xu Xueyi and Xia Zucun, 2000. Volcanism and resource effect in north Qilian ancient ocean basin. Abstracts of the Second Cross-Strait Conference on Geology of the Qilian Mountains and Adjacent Areas, 105-108.[43]Xiao Xuchang, Chen Guoming and Zhu Zhizhi, 1978. A preliminary study on the tectonics of ancient ophiolites in the Qilian Mountains, northwest China. Acta Geologica Sinica, 52 (4): 281-295 (in Chinese with English abstract).[44]Xiao Xuchang and Li Tingdong, 1995. Tectonic evolution and uplift of the Qinghai-Tibet plateau. Episodes, 18(1-2): 31-35.[45]Xu Jifeng, Yu Xueyuan, Li Xianhua et al., 2000. Geochemistry of the Anzishan ophiolite mé1ange in the Mian-Lüe belt of Qinling Orogen-evidence and implication of the Palaeo ocean crust. Acta Geologica Sinica, 74(1): 39-50 (in Chinese with English abstract).[46]Xu Ronghua, Harris, N.B.W., Lewis, C.L. Et al., 1990. Isotope geochemistry of the 1985 Tibet Geotraverse, Lhasa to Golmud. In: The Geological Evolution of Tibet. Beijing: Science Press, 282-302 (in Chinese).[47]Xu Ronghua, Zhang Yuquan, Xie Yingwen et al., 1994. A discovery of an Early Palaeozoic tectono-magmatic belt in the northem part of West Kunlun Mountains. Scientia Geologica Sinica, 29(4): 313-328 (in Chinese with English abstract).[48]Xu Zhiqin, Xu Huifeng, Li Haibing et al., 1994. The Zhoulang Nanshan Caledonian subductive complex in the Northern Qilian Mountains and its dynamics. Acta Geologica Sinica, 7 (3): 225-241.[49]Xu Zhiqin, Yang Jingshui and Cheng Fangyuan. 1996. The A'nyemaqen suture zone and the dynamics in subduction and collision. In: Zhang Qi (ed.), Study on Ophiolites and Geodynamics. Beijing: Geological Publishing House, 185-189 (in Chinese).[50]Xu Zhiqin, Yang Jingshui, Zhang Jianxin et al., 1999. A comparison between the tectonic units on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing. Acta Geologica Sinica, 73(3): 193-205 (in Chinese with English abstract).[51]Yang Hongyi, 2000. Laohushan fossil back-arc basin in eastern section of the Qilian fold belt, NW China. Abstracts of the Second Cross-Strait Conference on Geology of the Qilian Mountains and Adjacent Areas, 130-133.[52]Yang Jingshui, Xu Zhiqin, Li Haibing et al., 1998. Discovery of eclogite at northern margin of Qaidam Basin, NW China. Chinese Science Bulletin (English edition), 43(20): 1755-1760.[53]Yang Jingshui, Xu Zhiqin, Song Shuguang et al., 2000. Discovery of eclogite in Dulan, Qinghai Province and its significance for studying the HP-UHP metamorphic belt along the Central Orogenic Belt of China. Acta Geologica Sinica, 74(2): 156-168 (in Chinese with English abstract).[54]Yang Jingshui, Robinson, P T, Jiang Chunfa et al., 1996. Ophiolites of the Kunlun Mountains, China and their tectonic implications. Tectonophysics, 258: 215-231.[55]Yin Hongfu, Du Yuansheng, Xu Jifeng et al., 1996. Discovery of radiolarian fauna in Mianlte suture zone and its palaeo-ocean significance, South Qinling Mountains. Earth Science Journal of China University of Geosciences, 21(2): 184 (in Chinese with English abstract).[56]Yin Hongfu and Zhang Kexin, 1998. Evolution and characteristics of the Central Orogenic Belt. Earth Science-Journal of China University of Geosciences, 23(5): 437-442 (in Chinese with English abstract).[57]Yin Hongfu, Wu Shunbao, Du Yuansheng et al., 1999. South China defined as part of Tethyan archipelagic ocean system. Earth Science-Journal of China University of Geosciences, 24(1): 1-1 l (in Chinese with English abstract).[58]Zhang Chengli, Zhou Dingwu, Jin Hailong et al., 1999. Study on the Sr, Nd, Pb and O isotopes of basic dyke swarms in the Wudang block and basic volcanics of the Yaolinghe Group. Acta Petrologica Sinica, 15(3): 430-437 (in Chinese with English abstract).[59]Zhang Guowei, Meng Qingren, Yu Zhaiping et al., 1996. Orogenic processes and dynamics of the Qinling. Science in China (Series D) (English edition), 39(3): 225-234.[60]Zhang Guowei and Liu Xiaoming, 1998. Some remarks on China Central Orogenic System. Earth Science-Journal of China University of Geosciences, 23(5): 443-448 (in Chinese with English abstract).[61]Zhang Jianxin, Xu Zhiqin, Xu Huifeng and Li Haibing, 1998. Framework of North Qilian Caledonian subduction accretionary wedge and its deformation dynamics. Scientia Geologica Sinica, 33(3):290-299 (in Chinese with English abstract).[62]Zhang Qi, Sun Xiaomeng, Zhou Dejin et al., 1997. The characteristics of North Qilian ophiolites, forming setting, and their tectonic significance. Advance in Earth Sciences, 12(4): 366-393 (in Chinese with English abstract).[63]Zhang Qi and Zhou Guoqing, 2000. Ophiolites of China. Beijing: Science Press, 56-57 (in Chinese with English abstract).[64]Zhang Zongqing, Liu Dunyi, Fu Guomin et al., 1994. Isotopic Geochronology Study on Metamorphic Strata in the North Qinling Mountains. Beijing: Geological Pubulishing House, 191 (in Chinese).[65]Zhang Zongqing, Zhang Guowei, Fu Guomin et al., 1996. Geochronology of metamorphic strata in the Qinling Mountains and its tectonic implications. Science in China (series D) (English edition), 39(3): 283-292[66]Zhang Zhaocong, Mao Jingwen, Yang Jianmin et al., 1998. Geochemical evidences on the petrogenesis of the Aoyougou ophiolite in North Qilian Mountains. Acta Geologica Sinica, 72 (1): 42-51 (in Chinese with English abstract).[67]Zhang Zhiyong, Wang Jin, Gu Fengbao and Liu Yongcheng, 1998. Features of granite in the orogenic belt. Regional Geology of China (Suppl.), 56-61 (in Chinese).[68]Zhao, X.X., Coe, R.S., Liu, C., and Zhou, Y.X., 1992. New Cambrian and Ordovician palaeomagnetic poles for the North China block and their palaeo-geographic implications. J. Geophys. Res. 97, 1767-1788.[69]Zhou Dingwu, Dong Yunpeng, Liu Liang et al., 1998. Nd, Sr and Pb isotopic characteristics of the Proterozoic ophiolite from Songshugou area. Scientia Geologica Sinica, 33(1): 31-38 (in Chinese with English abstract).[70]Zhou Dingwu, Zhang Chengli, Liu Liang et al., 2000. Synthetic study on Proterozoic basic dyke swarms in the Qinling Orogenic Belt and its adjacent block as well as a discussion about some questions related to them. Acta Petrologica Sinica, 16(1): 22-28 (in Chinese with English abstract).[71]Zhu Yunhai, Zhang Kexin, Pan Yuanming et al., 1999. Determination of different ophiolitic belts in Eastern Kunlun orogenic zone and their tectonic significance. Earth Science, 24(2) 134-138 (in Chinese with English abstract). | BIAN Qiantao, GAO Shanlin, LI Dihui, YE Zhengren, CHANG Chengfa, LUO Xiaoquan Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029 Science Press, Chinese Academy of Sciences, Beijing 100717 | 2001 | Acta Geologica Sinica(English Edition)2001,75,4: | 19 |
| 18 | Laser altimetry data of Chang'E-1 and the global lunar DEM model显示文摘The Laser AltiMeter (LAM), as one of the main payloads of Chang'E-1 probe, is used to measure the topography of the lunar surface. It performed the first measurement at 02:22 on November 28th, 2007. Up to December 4th 2008, the total number of measurements was approximately 9.12 million, covering the whole surface of the Moon. Using the LAM data, we constructed a global lunar Digtal Elevation Model (DEM) with 3 km spatial resolution. The model shows pronounced morphological characteristics, legible and vivid details of the lunar surface. The plane positioning accuracy of the DEM is 445 m (1σ), and the vertical accuracy is 60 m (1σ). From this DEM model, we measured the full range of the altitude difference on the lunar sur-face, which is about 19.807 km. The highest point is 10.629 km high, on a peak between crater Korolev and crater Dirichlet-Jackson at (158.656°W, 5.441°N) and the lowest point is -9.178 km in height, inside crater Antoniadi (172.413°W, 70.368°S) in the South Pole-Aitken Basin. By comparison, the DEM model of Chang'E-1 is better than the USA ULCN2005 in accuracy and resolution and is probably identical to the DEM of Japan SELENE, but the DEM of Chang'E-1 reveals a new lowest point, clearly lower than that of SELENE. | LI ChunLai1, REN Xin1, LIU JianJun1, ZOU XiaoDuan1, MU LingLi1, WANG JianYu2, SHU Rong2, ZOU YongLiao1, ZHANG HongBo1, Lü Chang1, LIU JianZhong1, ZUO Wei1, SU Yan1, WEN WeiBin1, BIAN Wei1, WANG Min1, XU Chun1, KONG DeQing1, WANG XiaoQian1, WANG Fang1, GENG Liang1, ZHANG ZhouBin1, ZHENG Lei1, ZHU XinYing1, LI JunDuo1 & OUYANG ZiYuan1 1 National Astronomical Observatories, Chinese Academy of Sciences, Beijing 100012, China 2 Shanghai Institute of Technical Physics, Chinese Academy of Sciences, Shanghai 200083, China | 2010 | Science China Earth Sciences2010,53,11: | 19 |
| 19 | Comparison of endoscopic submucosal dissection with surgical gastrectomy for early gastric cancer: An updated meta-analysis显示文摘BACKGROUND There are several surgical options for treating early gastric cancers(EGCs), such as endoscopic resection, laparoscopic or open gastrectomy with D1 or D2 lymphadenectomy. Endoscopic resection for EGC with low risk of lymph node metastasis has been widely accepted as a therapeutic alternative. The role of endoscopic submucosal dissection(ESD) in treating EGC is not well established,especially when compared with resection surgery cases in a long-term follow-up scope.AIM To compare the safety and efficacy of the short-and long-term outcomes between ESD and resection surgery.METHODS We searched the databases of PubMed, EMBASE, Web of Science, and the Cochrane Library from January 1990 to June 2018, enrolling studies reporting short-or long-term outcomes of ESD in comparison with resection surgery for EGC. The quality of the studies was assessed by the Newcastle-Ottawa Quality Assessment Scale. Stata software(version 12.0) was used for the analysis. Pooling analysis was conducted using either fixed-or random-effects models depending on heterogeneity across studies.RESULTS Fourteen studies comprising 5112 patients were eligible for analysis(2402 for EGC and 2710 for radical surgery). Our meta-analysis demonstrated that the ESD approach showed advantages through decreased operation time [weighted mean difference(WMD):-140.02 min, 95%CI:-254.23 to-34.82 min, P = 0.009], shorter hospital stay(WMD:-5.41 d, 95% CI:-5.93 to-4.89 d, P < 0.001), and lowerpostoperative complication rate [Odds ratio(OR) = 0.39, 95%CI: 0.28-0.55, P <0.001). Meanwhile, EGC patients who underwent ESD had higher recurrence rate(OR = 9.24, 95%CI: 5.94-14.36, P < 0.001) than resection surgery patients.However, the long-term survival including overall survival [Hazard ratio(HR) =0.51, 95%CI: 0.26-1.00, P = 0.05] and event-free survival(HR = 1.59, 95%CI: 0.66-9.81, P = 0.300) showed no significant differences between these two groups.CONCLUSION In the treatment of EGC, ESD was safe and feasible in comparison with resection surgery, with advantages in several surgical and post-operative recovery parameters. Although the recurrence rate was higher in ESD group, the longterm survival was still comparable in these two groups, suggesting ESD could be recommended as standard treatment for EGC with indications. | Hua Li Li-Qian Feng Yao-Yao Bian Li-Li Yang Deng-Xiang Liu Zhi-Bin Huo Li Zeng | 2019 | World Journal of Gastrointestinal Oncology2019,11,2: | 17 |
| 20 | Advances in studying interactions between aerosols and monsoon in China显示文摘Scientific issues relevant to interactions between aerosols and the Asian monsoon climate were discussed and evaluated at the 33 rd 'Forum of Science and Technology Frontiers' sponsored by the Department of Earth Sciences at the Chinese Academy of Sciences. Major results are summarized in this paper. The East Asian monsoon directly affects aerosol transport and provides a favorable background circulation for the occurrence and development of persistent fog-haze weather. Spatial features of aerosol transport and distribution are also influenced by the East Asian monsoon on seasonal, inter-annual, and decadal scales. High moisture levels in monsoon regions also affect aerosol optical and radiative properties. Observation analyses indicate that cloud physical properties and precipitation are significantly affected by aerosols in China with aerosols likely suppressing local light and moderate rainfall, and intensifying heavy rainfall in southeast coastal regions. However, the detailed mechanisms behind this pattern still need further exploration. The decadal variation in the East Asian monsoon strongly affects aerosol concentrations and their spatial patterns. The weakening monsoon circulation in recent decades has likely helped to increase regional aerosol concentrations. The substantial increase in Chinese air pollutants has likely decreased the temperature difference between land and sea, which favors intensification of the weakening monsoon circulation. Constructive suggestions regarding future studies on aerosols and monsoons were proposed in this forum and key uncertain issues were also discussed. | WU GuoXiong LI ZhanQing FU CongBin ZHANG XiaoYe ZHANG RenYi ZHANG RenHe ZHOU TianJun LI JianPing LI JianDong ZHOU DeGang WU Liang ZHOU LianTong HE Bian HUANG RongHui | 2016 | Science China Earth Sciences2016,59,1: | 16 |