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| 1 | Mesoproterozoic age for Xiamaling Formation in North China Plate indicated by zircon SHRIMP dating显示文摘Zircon grains of magmatic origin from tuffite layers in the Xiamaling Formation at Zhaojiashan Village, Xuanhua area, Hebei Province, were used for zircon dating with a Sensitive High-Resolution Ion Microprobe (SHRIMP II), which gives a weighted mean 207Pb/206Pb age of 1366±9 Ma. It shows a very similar age (1368±12 Ma) as the zircon dating from the Xiamaling Formation in Western Hill, Beijing. This age proposes that the Xiamaling Formation in the North China plate should be of Mesoproterozoic, instead of Neoproterozoic based on K-Ar, Ar-Ar dating. The new zircon age also indicates the devel- opment of macrofossils algae from the Mesoproterozoic age. | GAO LinZhi ZHANG ChuanHeng SHI XiaoYing SONG Biao WANG ZiQiang LIU YaoMing | 2008 | Chinese Science Bulletin2008，53，17： | 68 |
| 2 | Petrogenesis and dating of the Kangding complex,Sichuan Province显示文摘An analysis of major and trace element geochemistry and SHRIMP U-Pb zircon dating of mafic, intermediate, and felsic rocks from the Mianning metamorphic complex of Si- chuan Province was conducted. One of our conclusions is that a majority of the zircons crystal- lized between 721 and 773 Ma in a magmatic regime. The complexes contain early to late Pa- leo-proterozoic relict zircons from ancient continental crust. The oldest age, 2468 Ma, may rep- resent the basement of the Yangtze block. Overgrowth zircon rims and palingenetic zircons have been observed and dated, and are believed to have formed after crystallization, during Paleozoic and Mesozoic metamorphic-anatexis. We also conclude that depletion of Nb, Ta, HREE, in a spider-diagram normalized to primitive mantle and calc-alkaline association, implies that they formed in island-arc or under-plating settings. | CHEN Yuelong 1 , LUO Zhaohua 1 , ZHAO Junxiang, LI Zhihong, ZHANG Hongfei & SONG Biao 3 1. Faculty of Earth Sciences and Natural Resources, China University of Geosciences, Beijing 100083, China 2. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China 3. Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China | 2005 | Science China Earth Sciences2005，48，5： | 40 |
| 3 | Seismic Sequence in Carbonate Rocks By Vibrational Liquefaction显示文摘On the basis of the records of strong seismic events taking place in soft carbonate sediments, a new seismic sequence system of vibrational liquefaction is established, which consists of a series of units, such as escaped structure of micrite veins and liquefied deformation formed in the period of seismic liquefaction, land subsidence structure after liquefaction, tsunamic hummocky and turbidite produced by seismic events, This sequence is a generalization and summation of field observation in vast areas, which shows the whole process of a strong seismic event and provides an unified theoretical explanation. The pattern of the seismic sequence by vibrational liquefaction provides one of correlation standards for geologists in the field to discriminate events in carbonate sequences. Based on the pattern of seismic sequence, the authors first advance a new conception of the Palaeo-Tanlu (Tancheng-Lujiang) Zone and discuss primarily its geological significations. | Qiao Xiufu, Song Tianrui, Gao Linzhi, Peng Yang, Li Haibing, Gao Mai, Song Biao and Zhang QiaodaInstitute of Geology, Chinese Academy of Geological Sciences, Beijing | 1994 | Acta Geologica Sinica(English Edition)1994，68，3： | 39 |
| 4 | Zircon U-Pb dating for the earliest Neoproterozoic mafic magmatism in the southern margin of the North China Block显示文摘Huge diabase occurs within the Pro- terozoic strata in the southern margin of the North China Block, geographically in the northern parts of Anhui and Jiangsu provinces, where no strata younger than Neoproterozoic have been found. Zir- cons from the diabase show three different structures from cathodoluminesecence imaging, but they are all of magmatic origin. SHRIMP U-Pb dating yields a range of 206Pb/238U ages from 2600 to 124 Ma, but two geological events can clearly be identified from both concordant and discordant ages. One gives two weighted mean 207Pb/206Pb ages of 976 ± 24 and 1038 ± 26 Ma which are interpreted as timing of dia- base crystallization, and the other has a weighted mean 207Pb/206Pb age of 2523 ± 52 Ma that repre- sents formation time of inherited zircon from the old crust. The dating results indicate that the mafic magmatic event occurred in a transition period from the latest Mesoproterozoic to the earliest Neopro- terozoic, consistent with global subduction of Grenvill ocean crust to result in the assembly of superconti- nent Rodinia. Therefore, the North China Block needs to be taken into account when reconstructing the position of China continents within the framework of Rodinia supercontinent. | LIU Yongqing GAO Linzhi LIU Yanxue SONG Biao WANG Zongxiu | 2006 | Chinese Science Bulletin2006，51，19： | 36 |
| 5 | Reclassification of the Meso- and Neoproterozoic Chronostratigraphy of North China by SHRIMP Zircon Ages显示文摘High-quality zircon U-Pb ages acquired from Meso- and Neoproterozoic strata in North China in recent years has provided a high-resolution chronostratigraphic framework for dating. A basis of this high-level chronostratigraphic system provides the foundation for a global Precambrian study and stratigraphic correlation and so recent geological studies have focused attention on systemic SHRIMP zircon dating. A chronology of Meso- and Neoproterozoic strata and the time of origin of the overlying Changcheng System is given on the basis of new SHRIMP zircon dating from the Qianxi Complex and diabase of the Chuanlinggou Formation. A new tectonostratigraphy for a Neoproterozoic chronostratigraphic framework in the southeastern margin of the North China continent is underpinned by the new SHRIMP zircon dating of a Neoproterozoic mafic magma diabase in the Jiao-Liao-Xu-Huai Sub-Province. | GAO Linzhi ZHANG Chuanheng LIU Pengju TANG Feng SONG Biao DING Xiaozhong | 2009 | Acta Geologica Sinica(English Edition)2009，83，6： | 36 |
| 6 | Geochronology of Baogutu porphyry copper deposit in Western Junggar area, Xinjiang of China显示文摘Baogutu copper deposit in Western Junggar area is a mesoscopic porphyry deposit found in recent years. Study on its geochronology will help further understand ore genesis and regional ore-forming pattern. A series of small quartz-diorite and granodiorite stocks outcrop at Baogutu area, numbered I―X according to their size. A detailed exploration on Number V stock confirmed it as a mesoscopic scale copper deposit, and various exploration work has been carried out on other stocks with ore-forming evidence. This paper studies geochronology of Number V stock using zircon SHRIMP U-Pb and single mineral K-Ar method. Twenty-five SHRIMP ages yield two 206Pb/238U weighed mean ages of 335.6 ± 7.8 Ma and 311.4 ± 3.3 Ma respectively. The older date is considered to be inherited zircon from either surrounding rock tuff or deep granitoid batholith, whereas the younger date is the formation age of ore-bearing intrusion. K-Ar ages of ore-forming biotites, 296.0 ± 3.7 Ma and 297.3 ± 3.8 Ma, in combination with Re-Os age of molybdenite, 310 Ma, confirm the ore-forming age of 310-296 Ma. Granophyre and dioritic porphyrite dikes cut Number V stock and their K-Ar ages range from 278 to 240 Ma, which confine the lower boundary of the mineralization. The framework of Baogutu ore-forming geochrono-logy can be established based on these data. | LIU YuLin GUO LiShuang LIU YuDe SONG HuiXia SONG Biao ZHANG Rui XU FaJun ZHANG YunXiao | 2009 | Science China Earth Sciences2009，52，10： | 33 |
| 7 | Early Paleozoic granite in Nujiang River of northwest Yunnan in southwestern China and its tectonic implications显示文摘沿着在西方的云南的中国缅甸边阶的 Nujiang 区域收到了很多注意并且被认为是西藏的高原的向东南的逃跑的重要隧道。这条隧道被红 River-Ailao 山左文字的 strick 滑倒差错在这条隧道以内在西方在东方和英雄传奇 Gaoligong 正确文字的 strick 滑倒差错毗邻,它仍然不对贡尚·布洛克哪个构造单位合适清楚。尽管一些研究人员建议它是 Sundaland 岩层的北方结束,它的构造定义是相当模糊的。这篇论文报导我们 U-Pb 同位素的 geochronological 在贡尚·布洛克以内在 Gudang 片麻岩的花岗石上学习的新锆石。这研究在理解起源和西北的云南的构造环境起一个重要作用。 | SONG ShuGuang JI JianQing WEI ChunJing SU Li ZHENG YaDong SONG Biao ZHANG LiFei | 2007 | Chinese Science Bulletin2007，52，17： | 31 |
| 8 | Regulating effects of arsenic trioxide on cell death pathways and inflammatory reactions of pancreatic acinar cells in rats显示文摘背景煽动性的 cytokines 在尖锐胰腺炎的发展起一个关键作用,这被接受,那么堵住煽动性的反应的开始可以减轻尖锐胰腺炎的病理学的变化。我们在 vitro 在胰腺的 acinar 房间的 apoptosis 和 oncosis 上学习了砷三氧化物(As2O3 ) 的规章的效果,在尖锐 pancreatitis.Methods 上的 vivo 和它的治疗学的效果,胰腺的 acinar 房间被 collagenase 消化方法孤立。孤立的胰腺的 acinar 房间的 Apoptosis 和 oncosis 与 Hoechst 33258+PI 或 Annexin V+PI 被检测两倍荧光灯的染色。淀粉酶并且喂奶脱氢酶版本被测量。尖锐胰腺炎被 caerulein 的 intraperitoneal 注射在 Wistar 老鼠导致,并且 apoptosis 与把方法标记的终端 dUTP 刻痕结束被检测。肿瘤 necorsis 因素(TNF-) mRNA, myeloperoxidase,原子 factor-B 并且胰腺的损坏的组织学的分级是在那里的 measured.Results 是增加的 apoptosis 但是在有 As2O3 的处理以后的胰腺的 acinar 房间的减少的 oncosis。层次喂奶脱氢酶和淀粉酶版本显著地在在对待的 As2O3 的对待的 group.Myeloperoxidase 内容,TNF- mRNA 水平,原子 factor-B 激活和病理学的分数组织的 As2O3 被减少比在未经治疗的 group.Conclusions As2O3 能导致 apoptosis 和胰腺的 acinar 的还原剂 oncosis 的显著地低房间,因此导致 acinar 房间的 endocellular 酶的减少的版本,减少了煽动性的房间渗入并且减少 inflamma | XUE Dong-bo ZHANG Wei-hui YUN Xiao-guang SONG Chun ZHENG Biao SHI Xing-ye WANG Hai-yang | 2007 | Chinese Medical Journal2007，，8： | 26 |
| 9 | SHRIMP U-Pb Zircon Geochronology of the Xiaotongguanshan and Shatanjiao Intrusions and Its Petrological Implications in the Tongling Area, Anhui显示文摘This paper determines the crystallization ages of the Xiaotongguanshan quartz monzodiorite and Shatanjiao quartz monzonite porphyry from the Tongling area using the SHRIMP zircon U-Pb method. The crystallization age of the former is 142.8±1.8 Ma; that of the latter is 151.8±2.6 Ma. These data indicate that they were formed during the Late Jurassic (142.8 to 151.8 Ma). Zoned magma chamber was formed because of double diffusive convection. Therefore, the intrusive sequence of magma is generally from quartz monzonite through quartz monzodiorite to pyroxene monzodiorite, i.e. an inverted sequence. | DI Yongjun WU Ganguo ZHANG Da SONG Biao ZANG Wenshuan ZHANG Zhongyi LI Jinwen | 2005 | Acta Geologica Sinica(English Edition)2005，79，6： | 22 |
| 10 | Long-term results of endovascular therapy for proximal subclavian arterial obstructive lesions显示文摘背景 Endovascular 治疗是为锁骨下的动脉的局部性的吸藏的一种处理选择。在与 59 个病人一起的长期的经验是在1998年6月和2008年9月之间的 presented.Methods 的这份报告,我们使用了 endovascular 治疗在 59 个病人对待 61 锁骨下的动脉的妨碍的损害( 46 男性和 13 女性,有一个平均数的 34-82 岁变老( 61.9 眠瑩?佃?????????????? | WANG Ke-qin WANG Zhong-gao YANG Bao-zhong YUAN Chao ZHANG Wang-de YUAN Biao XING Tong SONG Sheng-han LI Tan LIAO Chuan-jun ZHANG Yang | 2010 | Chinese Medical Journal2010，，1： | 21 |
| 11 | Deterministic secure quantum communication over a collective-noise channel显示文摘We present two deterministic secure quantum communication schemes over a collective-noise. One is used to complete the secure quantum communication against a collective-rotation noise and the other is used against a collective-dephasing noise. The two parties of quantum communication can exploit the correlation of their subsystems to check eavesdropping efficiently. Although the sender should prepare a sequence of three-photon entangled states for accomplishing secure communication against a collective noise,the two parties need only single-photon measurements,rather than Bell-state measurements,which will make our schemes convenient in practical application. | GU Bin PEI ShiXin SONG Biao ZHONG Kun | 2009 | Science China(Physics,Mechanics & Astronomy)2009，52，12： | 20 |
| 12 | 5-Hydroxymethylcytosine signatures in cell-free DNA provide information about tumor types and stages显示文摘5-Hydroxymethylcytosine (5hmC ) 是被连接了到基因规定和癌症致病的重要哺乳动物的 DNA epigenetic 修正。这里,我们用定序途径的一枝敏感化学基于标签的低输入的猎枪在传播没有房间的 DNA (cfDNA ) 探索了 5hmC 的诊断潜力。我们从七种不同癌症类型的 49 个病人定序没有房间的 5hmC 并且发现了能被用来与高精确性预言癌症类型和阶段的不同特征。明确地,我们发现肺癌症在 cfDNA 导致 5hmC 的进步全球损失,而 hepatocellular 癌和胰腺的癌症在没有房间的 hydroxymethylome 导致疾病特定的变化。我们的 proof-of-principle 结果建议没有房间的 5hmC 签名可以潜在地被使用不仅识别癌症类型而且在一些癌症追踪肿瘤舞台。 | Chun-Xiao Song Senlin Yin Li Ma Amanda Wheeler Yu Chen Yan Zhang Bin Liu Junjie Xiong Weihan Zhang Jiankun Hu Zongguang Zhou Biao Dong Zhiqi Tian Stefanie S Jeffrey Mei-Sze Chua Samuel So Weimin Li Yuquan Wei Jiajie Diao Dan Xie Stephen R Quake | 2017 | Cell Research2017，27，10： | 17 |
| 13 | SHRIMP zircon U-Pb dating from K-bentonite in the top of Ordovician of Wangjiawan Section,Yichang,Hubei,China显示文摘The Global boundary Stratotype Section and Point (GSSP) for the base of the Hirnantian Stage (the latest stage of the Ordovician System) is defined at a point 0.39m below the base of the Kuanyinchiao Bed in the Wangjiawan North Section, which is the upper most 'golden spike' of the Ordovician. However, this 'golden spike' is lack of reliable geochronology data. This article gives a sensitive high resolution ion microprobe (SHRIMPII) zircon U-Pb dating for a K-bentonite sample from the Kuany-inchiao Bed in the Wangjiawan North Section. The age of the K-bentonite sample is 443.2±1.6 Ma, that is to say, the isotopic age of the uppermost of Hirnantian Stage, the point of Ordovician-Silurian boundary, should be near to, but slightly younger than 443.2±1.6 Ma. This age is identical to the Ordovi-cian-Silurian boundary age 443.7±1.5 Ma as declared by International Commission on Stratigraphy (ICS). So, this research provides some good geochronlogical data for the Hirnantian Stage and the Ordovician-Silurian boundary as well as the global correlation. | HU YanHua ZHOU JiBin SONG Biao LI Wei SUN WeiDong | 2008 | Science China Earth Sciences2008，51，4： | 15 |
| 14 | Identification of Rice Ethylene-Response Mutants and Characterization of MHZ71OsEIN2 in Distinct Ethylene Response and Yield Trait Regulation显示文摘乙烯在浸透水的环境在米饭植物的适应生长起必要作用;然而,在米饭的乙烯 signalingpathway 大部分是不清楚的。在这研究,我们在变白的米饭幼苗的特定的乙烯反应显型上报导乙烯反应 mutantsbased 的鉴定和描述,包括禁止乙烯的根生长支持 andethylene 的 coleoptile 延伸,它与乙烯不同在 Arabidopsis 的三倍反应的显型。我们证实为屏蔽和一套米饭异种的一个有效系统被识别了。基因分析 revealsthat 这些异种形成八个互补组。所有异种显示出 insensitivity 或减少的敏感到 ethylenein 根生长,但是在 coleoptile 生长展出微分回答。一变异的组 mhz7 在根和 coleoptile 生长有 insensitivity 到乙烯。我们由基于地图的 cloningmethod 识别了相应基因。MHZ7 编码对 EIN2 相应的膜蛋白质,在 Arabidopsis 发信号的乙烯的一个中央部件。在乙烯处理之上,变白 MHZ7-overexpressing 幼苗展出提高的 coleoptile 延伸,增加的 mesocotyl 生长和极其扭曲的短根,展示在米饭提高了乙烯反应显型。谷物长度在 MHZ7 转基因的植物被支持, 1000 谷物重量在 mhz7 异种被减少。衰老的过程也是的叶由 MHZ7 表示影响了。乙烯发信号的操作可以在 rice.Key 词改进适应生长和收益相关的特点: | Biao Ma Si-Jie He Kai-Xuan Duan Cui-Cui Yin Hui Chen Chao Yang Qing Xiong Qing-Xin Song Xiang LU Hao-Wei Chen dVan-Ke Zhang Tie-Gang Lu Shou-Yi Chen Jin-Song Zhang | 2013 | Molecular Plant2013，6，6： | 15 |
| 15 | Dynamics of saltwater intrusion in the Modaomen Waterway of the Pearl River Estuary显示文摘Observations indicate an abnormal characteristic of saltwater intrusion in the upper Modaomen Waterway of the Pearl River Estuary,i.e.,the maximum salinity occurs during the neap tide or the coming moderate tide instead of during the spring tide.To explore the associated dynamic mechanisms,a high resolution three-dimensional numerical model was set up based on the Finite Volume Coastal Ocean Model(FVCOM),which covered the entire river network,the Pearl River Estuary,and the adjacent sea.Numerical experiments illustrated that the upper Modaomen Waterway is significantly influenced by the saltwater intrusion from the Hongwan Waterway,a narrow and shallow channel connecting the Modaomen Waterway to the sea.Specific topography,spring-neap tidal variation,local wind stress,and their interaction drive an up-estuary residual current in the Hongwan Waterway,which is much stronger during the neap tide than during the spring tide.As a result,more saltwater in the Hongwan Waterway is spilled over into the Modaomen Waterway during the neap tide or the coming moderate tide.This is the inherent dynamic mechanism why the saltwater intrusion in the upper Modaomen Waterway reaches its maximum during the neap tide or the coming moderate tide.Besides,we also found that the winter prevailing wind can pronouncedly enhance the saltwater intrusion in the Modaomen Waterway. | WANG Biao ZHU JianRong WU Hui YU FuJiang SONG XueJia | 2012 | Science China Earth Sciences2012，55，11： | 12 |
| 16 | SHRIMP zircon U-Pb dating of the intrusives in the Tongling metallogenic cluster and its dynamic setting显示文摘This paper selected five typical Mesozoic intrusives from the Tongling metallogenic cluster (Xiaotongguanshan, Fenghuangshan, Xinqiao, Dongguashan, and Shatanjiao plutons), and made a systemic SHRIMP zircon U-Pb dating for the five plutons, which produced an age range of 151.8±2.6- 142.8±1.8 Ma. This work put an accurate constraint on the formation age of the intrusives in the Tongling metallogenic cluster. These age data indicate that magmatic activity reached a peak during Late Jurassic. The intrusive sequence of magma is generally from quartz monzonite (porphyry) through monzonite to granodiorite to quartz monzodiorite to pyroxene monzodiorite to gabbro-diabase. The intrusives of different lithology differed in crystallization age, probably implying the intrusives in the Tongling area underwent an evolutional process of magma, which was closely related to geodynamical setting in the depths of the area. A dynamic model was presented for the origin of the igneous rocks in the study area as follows. The assembly between the Yangtze craton and the North China craton fini- shed at the end of T3, and then the stage of another compressional orogeny began in the Tongling area, i.e., Pacific dynamic system. Along with the subduction of the Izanagi plate underneath the Eurasian plate at J2-J3, NW-trending compression toward the East China continent was produced, and compres- sional deformation also took place, forming NE-trending fold and resulting in thickening of the crust in the Tongling area. High-density eclogite-facies rocks were produced in the low part of the crust, re- sulting in the delamination of mantle lithosphere and lower crust, and upwelling of materials in as- thenosphere. Decompression melting produced basaltic magma, and the materials in lower crust were heated by the underplating of the basaltic magma. Thus, melting of lower crust yielded granitic magma, which intruded along deep and large faults through various geological processes (J3-K1). The SHRIMP U-Pb zircon age of 151.8±2.6-142.8±1.8 Ma for intrusives in the Tongling area suggests that the de- lamination of lithosphere mantle and lower crust at least began at middle-late stage of Late Jurassic, resulting in sharp thinning of lithosphere and intense extension of middle-upper crust. Thus, a lot of decollements were produced between cover and cover, basement and cover, and middle and lower crust. This was structural layering or detachment of lithosphere in the Tongling area. Three concordant ages for old inherited cores of magmatic origin (747-823 Ma) indicated that there were obvious mag- matism in the Tongling area during Neoproterozoic, and a little more of the Neoproterozoic igneous source rocks participated in the formation of Mesozoic intrusives. | GanGuo Wu Da Zhang YongJun Di WenShuan Zang XiangXin Zhang Biao Song ZhongYi Zhang | 2008 | Science China Earth Sciences2008，51，7： | 11 |
| 17 | Occurrence of Neoproterozoic low-grade metagranite in the western Beihuaiyang zone,the Dabie orogen显示文摘Based on detailed field investigations and petrographic observations,we discovered Neoproterozoic-emplaced granite from the metavolcanics of the Dingyuan Formation in the western Beihuaiyang zone,the Dabie orogen. This study reports the results of zircon U-Pb dating and preliminary petrographic observations on two metagranite samples. The studied rocks experienced epidote-amphibolite facies metamorphism and strong structural deformation. Their U-Pb ages are 726 ± 6 and 758 ± 12 Ma,respectively,similar to those for the Luzhenguan complex in the eastern segment of the Beihuaiyang zone. In combination with previously determined 635 ± 5 Ma low-grade metagabbro,this study suggests the occurrence of at least two types of Neoproterozoic intrusive rocks in the Beihuaiyang zone,the northern margin of the South China Block (SCB):726-758 Ma metagranite and 635 Ma metagabbro. These rocks occur within the metamorphosed Ordovician volcanic zone (originally named the Dingyuan Formation) and are in tectonic contact to each other,but they formed in different tectonic settings. The protolith ages for the Neoproterozoic low-grade metaigneous rocks are in good agreement not only with ages for two episodes of mid-and late-Neoproterozoic mafic and felsic magmatism in the Suizhou and Zaoyang area,Hubei Province,but also agree with protolith ages of ultrahigh-pressure metaigneous rocks in the Dabie-Sulu orogenic belt. In view of their tectonic relationships to country rocks,it appears that these Neoproterozoic low-grade rocks are exotic and they may have been detached and scraped from subducting SCB crust in the early Triassic during the initial continental subduction,and thrusted over Paleozoic metamorphosed rocks in the southern margin of the North China Block during continental collision. | LIU YiCan LIU LiXiang GU XiaoFeng LI ShuGuang SONG Biao | 2010 | Chinese Science Bulletin2010，55，30： | 10 |
| 18 | Detrital Zircon Dating of Meso-and Neoproterozoic Rocks in North China and Its Implications显示文摘从中央的新日期 -- 并且 Neoproterozoic 阶层贡献分会在 2009 年 11 月 24 日在中国的地层学上在前寒武纪的系统,和国家委员会上同意的中国的最近定义的前寒武纪的地层学的 timescale。首先, Changcheng 系统的年龄范围包括 Changzhougou, Chuanlinggou, Tuanshanzi 和 Dahongyu 形成被抑制了到 1.81.6 Ga。第二,包括 Gaoyuzhuang, Yangzhuang, Wumishan, Hongshuizhuang 和 Tieling 形成的 Jixian 系统被抑制了到 1.61.4 Ga。第三,一当还未命名(未定义) 系统(1.41.0 Ga ) 仅仅在 Jixian 节在 Xiamaling 形成被开发, Tianjing。第四, Qingbaikou 系统,包括 Luotuoling 和 Jing'eryu 形成被抑制了到 1.00.78 Ga。第五,在 780635 妈之间的 Nanhuan 系统范围,和 Sinian 系统在 635542 妈以内。然而,根据一系列虾, U-Pb 标明日期从在在华南站台的 Jiangnan Orogen 带晚前寒武纪,抑制阶层将作为在 Qingbaikou 系统的上面的部分被重新定义。帮助全球地球动力学,表示晚前寒武纪的节与是有用的统一,精确、高精确按年代先后的标明日期;这这里在诺思中国块和 Jiaoliao 朝鲜语块被定义。然而,在诺思中国的 Neoproterozoic Qingbaikou 学习将是在整个中央的影响 -- 并且在在在华南的扬采·布洛克和卡赛西亚·布洛克之间的 Jiangnan Orogenic 带的 Neoproterozoic。 | GAO Linzhi LIU Pengju YIN Chongyu ZHANG Chuanheng DING Xiaozhong LIU Yanxue SONG Biao | 2011 | Acta Geologica Sinica(English Edition)2011，85，2： | 9 |
| 19 | Parkin promotes proteasomal degradation of p62: implication of selective vulnerability of neuronal cells in the pathogenesis of Parkinson's disease显示文摘 | Pingping Song Shanshan Li Hao Wu Ruize Gao Guanhua Rao Dongmei Wang Ziheng Chen Biao Ma Hongxia Wang Nan Sui Haiteng Deng Zhuohua Zhang Tieshan Tang Zheng Tan Zehan Han Tieyuan Lu Yushan Zhu Quan Chen | 2016 | Protein & Cell2016，7，2： | 8 |
| 20 | Experimental study on strain and deformation monitoring of reinforced concrete structures using PPP-BOTDA显示文摘Pulse-prepump Brillouin optical time domain analysis (PPP-BOTDA) is a novel technique for distributed strain measurements, in which a pre-pump pulse is inputted in front of the measuring pump pulse to stimulate the phonon, so that higher spatial resolution and measurement precision can be obtained. Principle, methodologies and technical parameters of the PPP-BOTDA are presented and the influence of temperature on measurements is discussed. Applications are made in the bond test of steel rebars and the bending test of concrete girders. Test results show that the PPP-BOTDA can provide a precise description on the strain distribution of steel rebar and concrete, exhibiting the ability for crack detection. Moreover, structural deformation can be obtained indirectly by accumulating the distributed strains along the optical fiber, thus the deflection curves of the concrete girder during the loading process are obtained. Suggestions with regards to the application of the PPP-BOTDA in strain measurements and crack monitoring for civil infrastructures are given. | GUO Tong LI AiQun SONG YongSheng ZHANG Biao LIU Yang YU NingSheng | 2009 | Science China(Technological Sciences)2009，52，10： | 7 |
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