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| 1 | Spatial patterns and driving forces of land use change in China during the early 21st century显示文摘Land use and land cover change as the core of coupled human-environment systems has become a potential field of land change science (LCS) in the study of global environmental change. Based on remotely sensed data of land use change with a spatial resolution of 1 km × 1 km on national scale among every 5 years, this paper designed a new dynamic regionalization according to the comprehensive characteristics of land use change including regional differentiation, physical, economic, and macro-policy factors as well. Spatial pattern of land use change and its driving forces were investigated in China in the early 21st century. To sum up, land use change pattern of this period was characterized by rapid changes in the whole country. Over the agricultural zones, e.g., Huang-Huai-Hai Plain, the southeast coastal areas and Sichuan Basin, a great proportion of fine arable land were engrossed owing to considerable expansion of the built-up and residential areas, resulting in decrease of paddy land area in southern China. The development of oasis agriculture in Northwest China and the reclamation in Northeast China led to a slight increase in arable land area in northern China. Due to the 'Grain for Green' policy, forest area was significantly increased in the middle and western developing regions, where the vegetation coverage was substantially enlarged, likewise. This paper argued the main driving forces as the implementation of the strategy on land use and regional development, such as policies of 'Western Development', 'Revitalization of Northeast', coupled with rapidly economic development during this period. | LIU Jiyuan ZHANG Zengxiang XU Xinliang KUANG Wenhui ZHOU Wancun ZHANG Shuwen LI Rendong YAN Changzhen YU Dongsheng WU Shixin JIANG Nan | 2010 | Journal of Geographical Sciences2010，20，4： | 154 |
| 2 | Spatiotemporal characteristics, patterns, and causes of land-use changes in China since the late 1980s显示文摘Land-use/land-cover 变化(LUCC ) 有连接到人和自然相互作用。瓷器 Land-Use/cover 数据集(CLUD ) 从 1980 年代末在 5 年的间隔定期被更新到 2010,与基于 Landsat TMETM+ 图象的标准过程。陆地使用动态区域化方法被建议分析主要陆地使用变换。在国家规模的陆地使用变化的空间与时间的特征,差别,和原因然后被检验。主要调查结果如下被总结。越过中国的陆地使用变化(LUC ) 在最后 20 年(19902010 ) 里在空间、时间的特征显示了一个重要变化。农田变化的区域在南方减少了并且在北方,而是仍然是的全部的区域增加了几乎未改变。回收农田从东北被转移到西北。布满建筑物陆地很快膨胀了,主要在东方被散布,并且逐渐地展开到中央、西方的中国。树林首先减少了,然后增加但是荒芜的区域是反面。草地继续减少。在中国的 LUC 的不同空间模式被发现在之间迟了第 20 世纪并且早第 21 世纪。原版 13 个 LUC 地区在一些地区被边界的变化由 15 个单位代替。包括的这些变化(1 ) 的主要空间特征加速的扩大布满建筑物在 Huang-Huai-Hai 区域,东南的沿海的区域,长江的中流区域,和四川盆登陆;(2 ) 从东北中国和东方内部蒙古在北方转移了陆地开垦到绿洲在西北中国的农业区域;(3 ) 从在到稻的东北中国的喂雨的农田的连续转变回答;并且(4 ) 为在内部蒙古,黄土高原,和西南的多山的区域的南部的农业牧剧的交错群落的格林工程的谷物的有效性。在最后二十年,尽管在北方的气候变化在农田影响了变化,政策规定和经济驱动力仍然是越过中国的 LUC 的主要原因。在第 21 世纪的第一十年期间,在陆地使用模式驾驶了变化的人为的因素从单程的陆地开发转移了强调到开发和保存。动态区域化方法被用来在单位的 zoning 边界,地区的内部特征,和生长和减少的空间模式分析变化。结果揭示了变化过程的模式,也就是 LUC 的过程和在在不同阶段的特征的地区性的差别。地区的生长和减少在这动态 LUC zoning,在统一边界的变化,和在前者和后者十年之间的变化紧张的特征期间被检验。在为在不同类型和陆地使用的不同区域的变化的陆地使用和原因的模式和过程之间的其他的转变的模式被探索。 | LIU Jiyuan KUANG Wenhui ZHANG Zengxiang XU Xinliang QIN Yuanwei NING Jia ZHOU Wancun ZHANG Shuwen LI Rendong YAN Changzhe WU Shixin SHI Xuezheng JIANG Nan YU Dongsheng PAN Xianzhang CHI Wenfeng | 2014 | Journal of Geographical Sciences2014，24，2： | 245 |
| 3 | Inhibition of SARS-CoV-2 (previously 2019-nCoV) infection by a highly potent pan-coronavirus fusion inhibitor targeting its spike protein that harbors a high capacity to mediate membrane fusion显示文摘The recent outbreak of coronavirus disease(COVID-19)caused by SARS-CoV-2 infection in Wuhan,China has posed a serious threat to global public health.To develop specific anti-coronavirus therapeutics and prophylactics,the molecular mechanism that underlies viral infection must first be defined.Therefore,we herein established a SARS-CoV-2 spike(S)protein-mediated cell-cell fusion assay and found that SARS-CoV-2 showed a superior plasma membrane fusion capacity compared to that of SARS-CoV.We solved the X-ray crystal structure of six-helical bundle(6-HB)core of the HR1 and HR2 domains in the SARS-CoV-2 S protein S2 subunit revealing that several mutated amino acid residues in the HR1 domain may be associated with enhanced interactions with the HR2 domain.We previously developed a pan-coronavirus fusion inhibitor,EK1,which targeted the HR!domain and could inhibit infection by divergent human coronaviruses tested,including SARS-CoV and MERS-CoV.Here we generated a series of lipopeptides derived from EK1 and found that EK1C4 was the most potent fusion inhibitor against SARS-CoV-2 S protein-mediated membrane fusion and pseudovirus infection with IC50s of 1.3 and 15.8 nM,about 241-and 149-fold more potent than the original EK1 peptide,respectively.EK1C4 was also highly effective against membrane fusion and infection of other human coronavirus pseudoviruses tested,including SARS-CoV and MERS-CoV,as well as SARSr-CoVs,and potently inhibited the replication of 5 live human coronaviruses examined,including SARS-CoV-2.Intranasal application of EK1C4 before or after challenge with HCoV-OC43 protected mice from infection,suggesting that EK1C4 could be used for prevention and treatment of infection by the currently circulating SARS-CoV-2 and other emerging SARSr-CoVs. | Shuai Xia Meiqin Liu Chao Wang Wei Xu Qiaoshuai Lan Siliang Feng Feifei Qi Linlin Bao Lanying Du Shuwen Liu Chuan Qin Fei Sun Zhengli Shi Yun Zhu Shibo Jiang Lu Lu | 2020 | Cell Research2020，30，4： | 81 |
| 4 | An Archean continental block in the Taihangshan and Hengshan regions: Constraints from geochronology and geochemistry显示文摘Recent research on the tectonothermal evolution and geochronology in the Fuping, Hengshan and Wutaishan metamorphic complexes, together with the discoveries of a high-pressure granulite belt in the northern margin of the North China Craton (NCC) and high-pressure metapelites in the Jingangku Group of the Wutaishan complex, suggests that there was a Neoarchean to Paleoproterozoic orogenic belt related to collision between the Eastern and Western continental blocks. Comparison of geological, geochronological, tectonothermal and geochemical data between the Fuping and Hengshan complexes suggests these two complexes most likely originated and evolved as a single lithotectonic domain (i.e., the Taihangshan-Hengshan block) during the early evolution of the North China Craton, probably as an active margin to the Eastern Continental Block. The Taihangshan-Hengshan block has been subjected to intensive and extensive tectono-magmatism and high-grade metamorphism related to collision between the Eastern and Western continental blocks at ~1.80 Ga. | LIU Shuwen , LI Jianghai, PAN Yuanming, ZHANG Jian and LI Qiugen(1. The Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China 2. Department of Geological Sciences, University of Saskatchewan, Saskatoon, SK S7N 5E2, Canada) | 2002 | Progress in Natural Science:Materials International2002，12，8： | 32 |
| 5 | Re-Os and U-Pb Geochronology of the Erlihe Pb-Zn Deposit,Qinling Orogenic Belt,Central China,and Constraints on Its Deposit Genesis显示文摘The Erlihe Pb-Zn deposit is an important mine of the Pb-Zn metallogenic zone in the South Qinling Orogen.It has been considered a sedimentary exhalative deposit in previous investigations because the ore body occurs concordantly at the transitional location of an upright fold.Re and Os isotopic analyses for paragenetic pyrites with sphalerite and galena from the ore body have been used to determine the timing of mineralization and to trace the source of metallogenic materials.The Re-Os isotopic data of four pyrite samples construct an isochron,yielding a weighted average age of 226±17 Ma(mean square weighted deviation=1.7),which is considered the main mineralization age.A dioritic porphyrite vein sample,showing weaker mineralization,was also dated using the SHRIMP zircon UPb isotopic method to constrain the youngest metallogenic age of the ore deposit,because it distributes along a group of tensional joints cutting not only the upright fold in the deposit field,but also the main ore bodies.The dioritic porphyrite sample yields a weighted mean ^(206)Pb/^(238)U age of 221±3 Ma,which is slightly younger than the Re-Os isotopic isochron age of the pyrites,considered as the upper age limit of the mineralization,namely the ending age of the mineralization.The Os isotopic compositions of sulfide minerals distribute within a range between Os isotopic compositions of the crust and the mantle, indicating that the ore deposit can be derived from magma-related fluid,and the metallogenic materials are most likely derived from the mixing source of the crust and the mantle.The Erlihe Pb-Zn deposit and associated dioritic porphyrite vein,important records of Qinling tectonic-magmatism-mineralization activities,were formed during the Triassic collisional orogeny processes. | ZHANG Fan LIU Shuwen LI Qiugen SUN Yali WANG Zongqi YAN Quanren YAN Zhen | 2011 | Acta Geologica Sinica(English Edition)2011，85，3： | 30 |
| 6 | Analysis of Pathological data of renal biopsy at one single center in China from 1987 to 2012显示文摘 | Zhang Xueguang Liu Shuwen Tang Li Wu Jie Chen Pu Yin Zhong Li Minxia Xie Yuansheng Cai Guangyan Wei Ribao Qiu Qiang Wang Yuanda Shi Suozhu Chen Xiangmei | 2014 | Chinese Medical Journal2014，，9： | 30 |
| 7 | Fusion mechanism of 2019-nCoV and fusion inhibitors targeting HR1 domain in spike protein显示文摘Very recently,a novel coronavirus,2019-nCoV,emerged in Wuhan,China and then quickly spread worldwide,resulting in>17,388 confirmed cases and 361 deaths as of 3 February 2020,thus calling for the development of safe and effective therapeutics and prophylatics.1,2 Similar to severe acute respiratory syndrome(SARS)-CoV,2019-nCoV belongs to lineage B betacoronavirus,and it has the ability to utilize human angiotensin-converting enzyme 2(ACE2)as a receptor to infect human cells. | Shuai Xia Yun Zhu Meiqin Liu Qiaoshuai Lan Wei Xu Yanling Wu Tianlei Ying Shuwen Liu Zhengli Shi Shibo Jiang Lu Lu | 2020 | Cellular & Molecular Immunology2020，17，7： | 27 |
| 8 | Nature of the Precambrian metamorphic blocks in the eastern segment of Central Tianshan:Constraint from geochronology and Nd isotopic geochemistry显示文摘Granitoid gneisses are widespread in Precambrian metamorphic blocks of eastern segment of the Central Tianshan Tectonic Zone, and they have intrusive contact relationships with their metamorphic sedimentary country rocks of Proterozoic Xingxingxia and Kawabulag groups. Zircon U-Pb ages from a granodioritic gneiss (IW11-1) and a parametamorphic schist (W05-9) are determined at the Weiya area. Euhedral prismatic zircons from the granodioritic gneiss (IW11-1) provide U-Pb isotopic discordia intercept ages of 1218±17 Ma and 426±26 Ma, respectively, and euhedral prismatic zircons from the parametamorphic schist (W05-9) display U-Pb isotopic discordia intercept ages of 1216±74 Ma and 290±15 Ma, respectively. A whole-rock Sm-Nd isotopic isochron is determined in augen granitoid gneiss samples at the Gang- gou-Kumishi area and we obtain the isochron age of 1142±120 Ma, and its ε Nd (t) = -4.3. These geochronological data suggest that these Precambrian metamorphic basement blocks within eastern segment of the Central Tianshan Tectonic Zone can be produced during 1140—1220 Ma, and occur a nearly homochronous metamorphism. Integrated to these geochronological data, Nd depleted mantle model ages (T DM ) and epsilon Nd(t) values of these granitoid gneiss samples indicate that they can derive from mixing in various scales both magmas from mantle and crust sources at a late Mesoproterozoic active continental margin tectonic environment. Similarity in geochronology, Sm-Nd isotopic geochemistry between Weiya-Xingxingxia, Pargangtag and Ganggou-Kumishi areas suggests that they could be a bigger uniform metamorphic basement block, which could be formed by the assembly of the supercontinent Rodinia and be separated by late geological processes. | LIU Shuwen,GUO Zhaojie,ZHANG Zhicheng,LI Qiugen & ZHENG Haifei The Key Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,China School of Earth and Space Sciences,Peking University,Beijing 100871,China | 2004 | Science China Earth Sciences2004，47，12： | 26 |
| 9 | Zircon SHRIMP geochronology and geochemistry of TTG rocks in Sushui Complex from Zhongtiao Mountains with its geological implications显示文摘在宗陶·布莱克复杂的 Sushui 的 tonalite-trondhjermite-granodiorite (TTG ) 岩石能根据他们的锆石 U-Pb 年龄被划分成二个系列, geochemical 特征一是 subduction 相关的(SR ) 并且其它碰撞相关(CR ) 。和另外的晚太古代的岛弧 magmatism, SR TTG 岩石由于在东方、西方的黑人之间的海洋的 subduction 被开发在晚太古代;当 CR TTG 岩石在变厚的外壳的环境形成了时。它在 Paleoproterozoic 对在东方、西方的块之间的碰撞正在作出回应。所有这些特征支持宗陶·布洛克是在诺思中国 Craton 的中间的 Trans 北方中国 Orogen 的部分的一个模型。 | TIAN Wei LIU Shuwen LIU Chaohui YU Shengqiang LI Qiugen WANG Yueran | 2006 | Progress in Natural Science:Materials International2006，16，5： | 24 |
| 10 | Geochemistry,Nd Isotopic Characteristics of Metamorphic Complexes in Northern Hebei:Implications for Crustal Accretion显示文摘北方中国古地台(NCC ) 的北边缘的中间的片断在 Damiao-Changshaoying 区域主要由变形太古代的 Dantazi 建筑群, Paleoproterozoic Hongqiyingzi 复杂 andunmetamorphosed gabbro-anorthosite-meta-alkaline 花岗石,以及变形迟了的 Paleozoicmafic 组成到 granitoid 岩石。~ 2 .49 Ga Dantazi 复杂 comprisesdioritic-trondhjemitic-granodoritic-monzogranitic 片麻岩在角闪岩变形了到 granulitefacies。石油化学的特征表明大多数岩石属于媒介--tohigh钾计算碱的系列,和显示Mg~#不到 40 ,衰退权利的 REE 模式没有到在使primitivemantle正常化的蜘蛛图的显然积极的 Eu 异例,显然否定的 Th , Nb , Ta 和 Ti 异例,到-0.03,和弄空的披风的ε_( Nd )(t) =+0.65 为agesT_( DM ) =2.78-2.71 Ga 建模。在岩石成因论的学习显示岩石从从在一个大陆人边缘背景的再循环的外壳的 mafic 岩石的部分融化从弄空的披风和 granitoid 岩浆在 mafic 岩浆之间混合的 magmatic 被形成。2.44-2.41 Ga Hongqiyingzi 建筑群被变形 mafic-granodioritic-monzogranitic 片麻岩统治,显示到 Dantazi 建筑群的类似的石油化学的特征,对高钾也就是中等计算碱的系列,和 mafic 岩石在 LILE,否定 Th, Nb, Ta, Zr 异例和积极 Panomalies 显示出明显的变化。并且另外的 granitiod 样品也展出否定 Th, Nb, Ta, P 和 Ti 异例。在 Hongqiyingzi 复杂表演的 Allrocks 没有 Eu 的衰退权利的 REE 模式异例。有ε _(Nd ) 的 Themetamorphic mafic 岩石(t)=-1.64 不能是有 granitoids 的一个相同 magmatic 系列有(t)+3.19 珍视到 +1.94 和 2.55-2.52 Ga 的 T_(DM ) 年龄的ε _(Nd ) 。Thesegranitic 岩石从在一个弧形列岛的外壳的 mafic 岩石设置的少年的部分融化从弄空的披风和岩浆从在 mafic 岩浆之间的混血儿发源。 11 妈 LatePaleozoic 变形 mafic 摇的所有 ~3 和相关花岗石的岩石显示出一个中等钾的 calc-alkalinemagmatic 进化系列,由高Mg~#,显然否定的 Th , Nb , Ta 异例和positive 描绘了 Sr 异例,从不到有ε_( Nd )的强烈否定的 Ti 异例和扁平的 REE 模式(t)= +8.42 ,暗示 mafic 岩浆从弄空的披风被导出。另外的花岗石的岩石不管多么被衰退权利的 REE 模式显然描绘没有到 positiveEu 异例,显著地低的ε_( Nd )(t)= -13.37 到-14.04,和T_( DM ) =1.97-1.96 Ga ,表明 granitoid 岩浆从在来自 ~3 的 mafic 岩浆之间的混血儿被导出 11 Madepleted 披风和 granitoid 岩浆从对早 Paleoproterozoic 太古代古老的外壳的再循环。象上述地质的 andgeochronological 结果一样的地球化学和 Nd 同位素的特征显示 NCC 的北边缘的中间的片断主要经历了四个外壳的生长事件从对太古代晚古生代,它被三个大陆人统治边缘的弧生长( ~2 .49 , ~2 .44 和 311 妈)除了与 post-collisional 扩展有关的 1.76-1.68 Gaepisode ,表明这的外壳的生长分割主要从弧生长和合并被产生到 NCC 大陆块。 | LIU Shuwen TIAN Wei Lü Yongjun LI Qiugen FENG Yonggang K. H. PARK Y. S. SONG | 2006 | Acta Geologica Sinica(English Edition)2006，80，6： | 21 |
| 11 | SHRIMP Zircon U-Pb Chronology and Geochemistry of the Henglingguan and Beiyu Granitoids in the Zhongtiao Mountains,Shanxi Province显示文摘Henglingguan 和 Beiyu 变形 granitoids,在 Zhongtiaoshan 前寒武纪的建筑群的西北分布式,包括 trondhjemites 和计算碱的 monzogranites,与太古代的 Zhaizi TTG 片麻岩显示恼人的接触。并且 Beiyu metamorphicgranitoids 主要由 trondhjemites 组成,在 Hujiayu 背斜褶层的核心分布式。分别地,标明日期加权平均值 ~(207 )Pb/~(206 ) Pb 变老的数据表演的新虾锆石 U-Pb 是为 Henglingguan 变形计算碱的 monzogranites 和 Beiyu metamorphictrondhjemites 的 2435.9 Maand 2477 妈并且揭示 600 妈继承了的~ 2 在 magmatic 锆石的核心。Whole-rockgeochemical 数据显示那所有 Henglingguan 和 Beiyu 变形 trondhjemites andcalc 碱的 monzogranites 属于遇见了铝土的中等钾、高钾的 calc-alkalineseries。这些岩石被相对高的全部的碱内容描绘(Na_2O+K_2O,在 to9.08% 上面) ,弄空的 Nb, Ta, P 和 Ti,和衰退权利的 REE 模式与对高 LREEs/HREEsfractionation 中等(吝啬的比率(La/Yb )_n = 25 ) 。在多元素蜘蛛图的 Henglingguan 和 Beiyu metamorphictrondhjemites 显示 negative Rb, Th 和 K 异例由原始披风使正常化。Sm-Nd 同位素的数据表明这些 granitoids 有起始的ε _(Nd ) 到 +2.4 和 Nd 的(t)=-1.2 弄空 T_(MD )= 的披风模型年龄 2622 马马。所有 thesegeochemical 特征显示这些 granitoids 在一条大陆边缘的弧被形成,并且 trondhjemites 主要从少年的部分融化发源玄武岩的材料并且然而, Henglingguan 变形计算碱的 monzogranites 源于在一条大陆边缘的弧下面在古老的外壳中材料再循环。花岗石的岩浆在他们的形成期间经历了污染和分离结晶。 | YU Shengqiang, LIU Shuwen*, TIAN Wei, LI Qiugen and FENG Yonggang The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education School of Earth and Space Sciences, Peking University, Beijing 100871 | 2006 | Acta Geologica Sinica(English Edition)2006，80，6： | 21 |
| 12 | Application of General Shear Theory to the Study of Formation Mechanism of the Metamorphic Core Complex:A Case Study of Xiaoqinling in Central China显示文摘The kinematic vorticity number and strain of the mylonitic zone related to the detachment fault increase from ESE to WNW along the moving direction of the upper plate of the Xiaoqinling metamorphic core complex (XMCC) and the geometry of quartz c-axis fabrics changes progressively from crossed girdles to single girdles in the same direction. Therefore, pure shear is dominant in the ESE part of the XMCC while simple shear becomes increasingly important towards WNW. However, the shear type does not change with the strain across the shear zone, thus the variation of shear type is of significance in indicating the formation mechanism. The granitic plutons within the XMCC came from the deep source and their emplacement was an active and forceful upwelling prior to the detachment faulting. The PTt path demonstrates that magmatism is an important cause for the formation of the XMCC. The formation mechanism of the XMCC is supposed to be active plutonism and passive detachment. Crustal thickening and magmatic | ZHANG Jinjiang ZHENG Yadong LIU Shuwen | 2000 | Acta Geologica Sinica(English Edition)2000，74，1： | 20 |
| 13 | Petrogenesis of Indosinian Granitoids in Middle-Segment of South Qinling Tectonic Belt:Constraints from Sr-Nd Isotopic Systematics显示文摘南方 Qinling 构造的带(SQTB ) 在 Shangzhou-Danfeng 和 Mianxian-Lueyang 缝术之间被定位。在它的中间的片断有很多早中生代 granitoid plutons,包括在在西南的东北,在中央部分的 Huayang-Wulong-Laocheng granitoid plutons,在西北的 Xiba granitoid pluton 和 Guangtoushan-Liuba granitoid plutons 的 Dongjiangkou-Zhashui granitoid plutons。这些 Indonisian granitoids 包含各种各样的规模 mafic 被外国领地包围的土地的一个团,它与他们的主人 granitoids 显示出有时清楚的边界和有时过渡的边界。这些 granitoids 也从 low-K tholeiite 系列展出 metaluminous 到 peraluminous 系列,通常更高的 Mg# 和大量石油化学,通过 mid-K 和 high-K,到 shoshonite 系列的计算碱的系列和支配的样品被归因于 mid-K 和 high-K 计算碱的系列。在 Sr-Nd 同位素的 systematics 和石油化学的详细分析表明可以有 Indonisian granitoid plutons 的地区性起始的 granitoid 岩浆,包括 Dongjiangkou-Zhashui , Huayang-Wulong-Laocheng , Xiba ,和 Guangtoushan-Liuba granitoid plutons ,它被岩浆的混血儿在各种各样的度生产,并且起始的岩浆在 SQTB 从披风和更低的大陆人外壳( LCC )来源被导出。起始的 granitoid 岩浆进一步在他们的炮兵阵地期间与上面的外壳的材料从 LCC,结晶化分别,和吸收做了与岩浆混合的岩浆在 SQTB 生产这些 granitoid plutons。这些 magmatism 过程是最可能的发生在大陆下面边缘的弧和 syn 碰撞到碰撞以后的构造背景。 | LIU Shuwen LI Qiugen TIAN Wei WANG Zongqi YANG Pengtao WANG Wei BAI Xiang GUO Rongrong | 2011 | Acta Geologica Sinica(English Edition)2011，85，3： | 20 |
| 14 | What Happened in the Trans-North China Orogen in the Period 2560-1850 Ma?显示文摘Trans 北方中国造山带(TNCO ) 是东方、西方的块沿着混合了形成一个协调 NorthChina 古地台(NCC ) 的一条 Paleoproterozic continent-continentcollisional 带。最近地质,结构,有在东方块的西方的边缘下面的海洋的岩石圈的东方指导俯冲的 geochemical 和 theorogen 沿着东方块的西方的边缘是大陆人边缘或日本类型弧的同位素的数据表演,由旧海洋与西方的块被分开,。在 2550-2520 妈, deepsubduction 引起了媒介降低的外壳的部分融化,生产被侵入进形成 granitoid plutons 在的外壳的上面的层次的丰富的 granitoid 岩浆低 --tomedium 等级花岗石绿岩岩层。在 2530-2520 妈,海洋的岩石圈的俯冲引起了披风楔的部分融化,它在弧在下地壳和普遍 mafic 和次要的 felsic 火山作用在 mafic 岩浆的 plating 下面导致了,形成绿岩集合的部分。普遍 mafic 驾驶到 felsic 火山作用的扩展在造山带导致了发展 ofback 弧或 intra 弧盆。在 2520-2475 妈,俯冲引起了形成大量 tonalitic-trondhjemitic-granodioritic (TTG ) 的下地壳的进一步偏爱的融化岩浆酌。背弧盆的在这时候后面的进一步的扩展,阵发性的 granitoidmagmatism 发生了,导致 2360 妈,的炮兵阵地~ 2 250 妈 2110-21760 妈和~ 2 在造山带的 050 Magranites。当代的火山沉积的岩石在背弧 orintra 弧盆发展了。在 2150-1920 妈,造山带经历了几前紧张的事件,一条海洋的山脉的可能到期的 tosubduction,导致是的 mafic 女同性恋的炮兵阵地随后变形了到角闪岩和媒介 -- 到高压的 mafic granulites。在 1880-1820 妈,在东方、西方的块之间的海洋被俯冲完全消费,并且关门海洋导致了 continent-arc-continent 碰撞,它引起了大规模推进和等斜褶皱并且搬运了一些岩石进更低的外壳的层次或上地幔形成 granulites 或 eclogites 。山峰变态被 exhumation/uplift 跟随,导致在岩石中的不对称褶皱和 symplectic 质地的普遍开发。 | Guochun ZHAO LIU Shuwen Min SUN LI Sanzhong Simon WILDE Xiaoping XIA Jian ZHANG Yanhong HE | 2006 | Acta Geologica Sinica(English Edition)2006，80，6： | 16 |
| 15 | U-Pb Zircon Dating of the Granitic Conglomerates of the Hutuo Group:Affinities to the Wutai Granitoids and Significance to the Tectonic Evolution of the Trans-North China Orogen显示文摘与在中间的最好、古典的剖面图 Trans 北方 ChinaOrogen 分割的邻近的 Fuping 和 Hengshan Complexesrepresents 联系的 Wutai 建筑群,通常划分了成东方、西方的块。Unconformably overlying Wutai andFuping 建筑群 Hutuo 组在这个区域被看作最年轻的岩石地层单位并且为解释前寒武纪的历史以及 theTrans 北方中国造山带的全面进化重要。在这个组的沉积岩的起源的知识的缺乏妨碍了 depositional 和构造意义的理解。LA-ICP-MS 被使用为花岗石的卵石获得 U-Pb 锆石年龄, Hutuo 组的最低岩石层位学的岩石,它,与结合了以前的岩石层位学, geochronological,结构、变形的数据,在沉积起源和这个区域的构造进化上提供新限制。Hutuo 的顺序从更低的底砾岩 andvolcaniclastic 岩石(Doucun 亚群) 向上组织范围,通过碎屑沉积物,板岩,白云石和云石(Dongye 亚群) ,到在顶(Guojiazhai 亚群) 的沙岩和集团企业。从在 Doucun 亚群底砾岩保存的花岗石的卵石的锆石给加权的mean~( 207 )在 2517 妈和 2566 妈之间的Pb/~( 206 ) Pb 年龄,它与为迟了的 ArcheanWutai Granitoids 的那些一样,显示卵石从 Wutai 花岗石的侵入( 2566-2515 妈)被导出。基于新数据和以前的研究,与在 Hutuo 组为 volcanics 获得的 2087 ±9 妈的火的锆石结晶化年龄结合了, Hutuo 组在在东方块的西方的边缘下面在西方的块的东方指导俯冲期间在 theWutai 弧后面发展了的subduction相关的制动火箭弧低岬盆环境被扔。这盆经历了长寿沉积并且最后在~ 1 期间关上了导致了北方中国古地台的最后的合并的 850 妈 collisional 事件。 | Jian ZHANG Guochun ZHAO LI Sanzhong Min SUN LIU Shuwen Xiaoping XIA Yanhong HE | 2006 | Acta Geologica Sinica(English Edition)2006，80，6： | 15 |
| 16 | Evaluating the Provenance of Metasedimentary Rocks of the Jiangxian Group from the Zhongtiao Mountain Using Whole-Rock Geochemistry and Detrital Zircon Hf Isotope显示文摘在这研究,整个岩石的 geochemical 和 Nd,同位素的数据,以及从 Jiangxian 的沉积岩石组织的 Palaeoproterozoic 元的由岩屑形成的锆石 Hf 同位素被介绍评估他们的起源和构造历史的特征。专业和踪迹元素作文比得上Archean以后上面的大陆人外壳( PA-UCC ),但是在 LILE 有细微丰富,与例外 C 和 Sr ,和在含铁和镁的元素的细微弄空, HFS 元素例如 Nb 和 Ta ,并且一些主要元素,例如 CaO 和 Na 2 O 。 geochemical 数据表明收集了沉积岩石经历了中间的来源与化学索引捱过的元从 72~78 的改变值,K交代作用的变化的度,和 post-depositional Na 的损失,以及可以忽略的排序,并且从捱过被导出主要, felsic 和 non-mafic 摇。到 Trans 北方中国 Orogen 和作为为元的最可能的来源, Jiangxian 的沉积岩石组织的北方中国 craton 的东方块的由岩屑形成的锆石点上的选择的陆 Hf 同位素的分析。然而,从北方中国 craton 的西方的块的岩屑的贡献能被排除。沉积可能在一个活跃大陆人边缘背景以内在背弧盆被扔。 | LI Qiugen CHEN Xu LIU Shuwen WANG Zongqi ZHOU Yingkui ZHANG Jian WANG Tao | 2009 | Acta Geologica Sinica(English Edition)2009，83，3： | 15 |
| 17 | Ages of the Laocheng Granitoids and Crustal Growth in the South Qinling Tectonic Domain,Central China:Zircon U-Pb and Lu-Hf Isotopic Constraints显示文摘Laocheng granitoid pluton 位于 Qinling erogenic 带的南方 Qinling 构造领域,南部的 Shaanxi 省,并且由石英闪长岩, granodiorite 和 monzogranite 主要组成。LA-ICP-MS 锆石 U-Pb 与阴极射线发光图象一起,同位素的标明日期表明石英闪长岩和 granodiorite 是从 220 妈的 emplaced 到 216 妈,当 monzogranite 是在 210 妈的 emplaced 时。在原处,锆石 Hf 同位素的分析证明从 8.1 的石英闪长岩和到 +1.3 的 granodiorite 范围的 Hf (t)价值,和单个阶段的 Hf 从 809 妈为年龄建模到 1171 妈,当 monzogranite 的 Hf (t)价值是 14.5 到 +16.7 和单个阶段的 Hf 时,从 189 妈为年龄建模到 1424 妈。这些 Hf 同位素的特征表明石英闪长岩, granodiorite 和 monzogranite 从混合从弄空的披风和更低的大陆的部分融化导出的岩浆被形成外壳的材料,并且在 Neoproterozoic ( 800 妈)和 Indosinian ( 210 妈)期间有大陆人外壳生长的二个阶段分别地,时代在 Qinling orogrnic 的南方 Qinling 构造领域系上带子,华中。 | YANG Pengtao LIU Shuwen LI Qiugen ZHANG Fan WANG Zongqi WANG Dongsheng WANG Ruiting YAN Quanren YAN Zhen | 2011 | Acta Geologica Sinica(English Edition)2011，85，4： | 15 |
| 18 | Metabolic engineering and flux analysis of Corynebacterium glutamicum for L-serine production显示文摘L-Serine plays a critical role as a building block for cell growth, and thus it is difficult to achieve the direct fermentation of L-serine from glucose. In this study, Corynebacterium glutamicum ATCC 13032 was engineered de novo by blocking and attenuating the conversion of L-serine to pyruvate and glycine, releasing the feedback inhibition by L-serine to 3-phosphoglycerate dehydrogenase (PGDH), in combination with the co-expression of 3-phosphoglycerate kinase (PGK) and feedback-resistant PGDH (PGDHr). The resulting strain, SER-8, exhibited a lower specific growth rate and significant differences in L-serine levels from Phase I to Phase V as determined for fed-batch fermentation. The intracellular L-serine pool reached (14.22±1.41) μmol gCDM 1, which was higher than glycine pool, contrary to fermentation with the wild-type strain. Furthermore, metabolic flux analysis demonstrated that the over-expression of PGK directed the flux of the pentose phosphate pathway (PPP) towards the glycolysis pathway (EMP), and the expression of PGDHr improved the L-serine biosynthesis pathway. In addition, the flux from L-serine to glycine dropped by 24%, indicating that the deletion of the activator GlyR resulted in down-regulation of serine hydroxymethyltransferase (SHMT) expression. Taken together, our findings imply that L-serine pool management is fundamental for sustaining the viability of C. glutamicum, and improvement of C1 units generation by introducing the glycine cleavage system (GCV) to degrade the excessive glycine is a promising target for L-serine production in C. glutamicum. | LAI ShuJuan ZHANG Yun LIU ShuWen LIANG Yong SHANG XiuLing CHAI Xin WEN TingYi | 2012 | Science China(Life Sciences)2012，55，4： | 15 |
| 19 | Paleoproterozoic Potassic Granitoids in the Sushui Complex from the Zhongtiao Mountains,Northern China:Geochronology,Geochemistry and Petrogenesis显示文摘Paleoproterozoic potassic granitoids in the southern Sushui Complex from the Zhongtiao Mountains yielded SHRIMP zircon U-Pb ages of 1968–1944 Ma. Lithologically, the potassic granitoid series consists chiefly of monzodiorite, quartz monzonite and syenogranite. Their trace elements and Sm-Nd isotope characteristics indicate that they were derived from partial melting of Archean TTG rocks in an overthickened continental crust. Petrogenesis of this potassic granitoid series implies a collisional environment within the Trans-North China Orogen in the Paleoproterozoic, which supports a tectonic model of Eastern and Western Continental Blocks being amalgamated in the Paleoproterozoic. | TIAN Wei LIU Shuwen ZHANG Huafeng | 2006 | Acta Geologica Sinica(English Edition)2006，80，6： | 14 |
| 20 | Xiba Granitic Pluton in the Qinling Orogenic Belt, Central China: Its Petrogenesis and Tectonic Implications显示文摘Xiba granitic pluton is located in South Qinling tectonic domain of the Qinling orogenic belt and consists mainly of granodiorite and monzogranite with significant number of microgranular quartz dioritic enclaves. SHRIMP zircon U-Pb isotopic dating reveals that the quartz dioritic enclaves formed at 214±3 Ma, which is similar to the age of their host monzogranite (218±1 Ma). The granitoids belong to high-K calc-alkaline series, and are characterized by enriched LILEs relative to HFSEs with negative Nb, Ta and Ti anomalies, and right-declined REE patterns with (La/Yb) N ratios ranging from 15.83 to 26.47 and δEu values from 0.78 to 1.22 (mean= 0.97). Most of these samples from Xiba granitic pluton exhibit εNd(t) values of 8.79 to 5.38, depleted mantle Nd model ages (T DM ) between 1.1 Ga and 1.7 Ga, and initial Sr isotopic ratios ( 87 Sr/ 86 Sr) i from 0.7061 to 0.7082, indicating a possible Meso-to Paleoproterozoic lower crust source region, with exception of samples XB01-2-1 and XB10-1 displaying higher ( 87 Sr/ 86 Sr) i values of 0.779 and 0.735, respectively, which suggests a contamination of the upper crustal materials. Quartz dioritic enclaves are interpreted as the result of rapid crystallization fractionation during the parent magmatic emplacement, as evidenced by similar age, texture, geochemical, and Sr-Nd isotopic features with their host rocks. Characteristics of the petrological and geochemical data reveal that the parent magma of Xiba granitoids was produced by a magma mingling process. The upwelling asthenosphere caused a high heat flow and the mafic magma was underplated into the bottom of the lower continent crust, which caused the partial melting of the lower continent crustal materials. This geodynamic process generated the mixing parent magma between mafic magma from depleted mantle and felsic magma derived from the lower continent crust. Integrated petrogenesis and tectonic discrimination with regional tectonic evolution of the Qinling orogen, it is suggested that the granitoids are most likely products in a post-collision tectonic setting. | ZHANG Fan LIU Shuwen CHEN Xu LI Qiugen DAI Junzhi YANG Kai WU Fenghui CHEN Youzhang | 2012 | Acta Geologica Sinica(English Edition)2012，86，5： | 13 |
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