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| 1 | 西天山东塔尔别克金矿区安山岩LA-ICP-MS锆石U-Pb年代学、元素地球化学与岩石成因显示文摘东塔尔别克金矿区位于西天山吐拉苏盆地内阿希金矿区南侧,构造上属于伊犁-中天山微板块与准噶尔板块之间的博罗科努早古生代岛弧带西段。东塔尔别克矿区出露有一些安山岩,这些岩石具有典型高镁安山岩特征,如高硅(SiO_2=58.94%~63.85%),具有较高的MgO含量(3.75%~6.59%)和Mg~#(58~69)、高的Cr(94.2×10^(-6)~241×10^(-6))、和Ni (54.5×10^(-6)~126×10^(-6))含量,以及低的FeO^T/MgO比值。除了Sr含量略微偏低(235×10^(-6)~696×10^(-6))之外,这些岩石基本显示了埃达克岩的地球化学特征:高的Al_2O_3(15.39%~16.65%),低Y(9.86×10^(-6)~14.9×10^(-6))含量,以及高的Sr/Y比值(23.8~48.1),无Eu异常,Nb、Ta、Ti亏损等。LA-ICP-MS锆石U-Pb测年结果显示安山岩的年龄为347.2±1.6Ma,为早石炭世。安山岩富集Rb、Th、U等大离子亲石元素,相对亏损Nb、Ta、Ti等高场强元素,轻重稀土元素分馏明显,具有俯冲带岛弧岩浆的特征。东塔尔别克安山岩可能形成于岛弧环境中,并可能由俯冲的晚古生代北天山洋洋壳以及少量上覆沉积物熔融形成,产生的熔体在上升过程中与地幔橄榄岩发生了相互作用.熔体-地幔相互作用对区内金矿的形成具有重要意义。 | 唐功建 王强 赵振华 Derek A WYMAN 陈海红 贾小辉 姜子琦 | 2009 | 岩石学报2009，25，6： | 27 |
| 2 | 西藏冈底斯南缘冲木达约30Ma埃达克质侵入岩的成因:向北俯冲的印度陆壳的熔融?显示文摘40~25 Ma之间通常被认为是拉萨地块特别是藏南冈底斯带岩浆活动的间歇期,与新特提斯洋板片断离后印度-亚洲大陆的硬碰撞有关。对出露于冈底斯东段南缘的冲木达石英二长岩-花岗闪长岩及相关的闪长质包体进行了锆石LA-ICPMS U-Pb定年和主微量元素、Sr-Nd同位素和锆石原位Hf同位素研究。年代学分析显示,侵入岩及其包体形成时代分别为(30.2±0.7)Ma和(31.0±0.5)Ma,近同时形成。冲木达侵入岩富硅(SiO2=64.56%~68.31%),高Sr(649~881μg/g),低Y(7.82~11.4μg/g)和Yb(0.78~1.04μg/g),Sr正异常,高场强元素亏损等,与典型埃达克岩的特征比较类似,但略微高钾(K2O=3.46%~4.10%)和微弱Eu负异常。其初始87Sr/86Sr比值为0.7057~0.7062,εNd(t)值为?3.34~?2.50,εHf(t)值为+2.2~+6.6。闪长质包体中高硅(SiO2=57.76%)样品显示了高镁(MgO=4.67%)、低Nb(15.1μg/g)和Nb/La(0.18)值的特点,但低硅(SiO2=54.76%)样品则低镁(MgO=3.47%)、高Nb(44.3μg/g)和Nb/La(0.68)值。除εNd(t)值(?4.08~?0.43)变化较大外,包体的初始87Sr/86Sr比值为0.7055~0.7062,εHf(t)变化于+0.7至+6.9之间,与埃达克质侵入岩类似。冲木达埃达克质侵入岩及其包体的形成很可能与俯冲陆壳熔融产生的熔体与地幔的相互作用有关:埃达克质侵入岩主要由早渐新世向北俯冲到拉萨地块下部的印度下地壳的熔融形成,高硅闪长质包体与俯冲陆壳熔体受到了上覆地幔橄榄岩的混染有关,低硅闪长质包体则可能由俯冲陆壳熔体交代的地幔部分熔融形成。另外,约30 Ma埃达克质侵入岩的出现可能表明,在拉萨地块南部,至少在约30 Ma,地壳已经增厚。 | 姜子琦 王强 WYMAN D.A. 唐功建 贾小辉 杨岳衡 喻亨祥 | 2011 | 地球化学2011，40，2： | 28 |
| 3 | Vacuum-Assisted Closure: A New Method for Wound Control and Treatment: Animal Studies and Basic Foundation显示文摘 | Michael J. Morykwas Louis C. Argenta Erica I. Shelton-Brown Wyman McGuirt | 1997 | Annals of Plastic Surgery1997，，6： | 8 |
| 4 | 表面深滚处理对AZ91镁合金组织及性能的影响(英文)显示文摘在室温下对固溶处理后的AZ91 镁合金块体材料进行表面深滚处理,以研究其对合金表面显微组织和力学性能的影响。分析被加工试样表层沿深度方向的显微硬度和显微组织。结果表明,表面影响层厚度达到2.0 mm,可分为3 个亚层:从最表面起约为400μm 厚的严重变形层,大约600μm 厚的中等变形层和厚度达1000μm 的小变形层。在变形层中除晶粒细化外,还观察到应变诱导析出的β相(Mg17Al12),尤其是在严重变形层和中等变形层内。研究认为,晶粒细化、应变硬化和沉淀强化的协同作用使AZ91 镁合金在表面深滚后的硬度显著提高。 | 罗贤 Qi-yang TAN Ning MO Yu YIN 杨延清 Wyman ZHUANG Ming-xing ZHANG | 2019 | Transactions of Nonferrous Metals Society of China2019，29，7： | 7 |
| 5 | Guidelines for the Echocardiographic Assessment of the Right Heart in Adults: A Report from the American Society of Echocardiography显示文摘 | Lawrence G. Rudski Wyman W. Lai Jonathan Afilalo Lanqi Hua Mark D. Handschumacher Krishnaswamy Chandrasekaran Scott D. Solomon Eric K. Louie Nelson B. Schiller | 2010 | Journal of the American Society of Echocardiography2010，，7： | 6 |
| 6 | 洋中脊或海岭俯冲与岩浆作用及金属成矿显示文摘扩张洋中脊、无震海岭或大洋高原和残余弧脊是现代海洋的重要组成部分,其面积超过当今世界海洋总面积的20~30%.它们均可以发生俯冲,可称为脊或海岭俯冲,这是现代大洋板块动力学系统中十分普遍且非常重要的一种地质过程,并可能与岛弧岩浆作用的产生及物质循环、大陆地壳生长与演化、上覆板块变形以及金属成矿相关,受到广泛关注.现代典型扩张洋中脊在正向或高角度俯冲时,会形成板片窗,并形成特殊的埃达克岩-高镁安山岩-富Nb玄武岩-洋岛玄武岩型或洋中脊玄武岩型玄武岩组合,且与金成矿关系密切.无震海岭或大洋高原由于其厚的地壳(大于正常洋壳厚度6~7km)、高的地形,传统上被认为很难发生俯冲或只能发生碰撞或平坦(低角度<10°)俯冲.但是,新生代太平洋东西两岸的无震海岭或大洋高原发生了俯冲,其中太平洋东岸无震海岭或大洋高原俯冲一般为平坦或相对小角度俯冲,这时往往会形成岩浆间歇期,但是在板片回卷或板片撕裂过程,板片会发生熔融,并形成一些埃达克岩或埃达克岩-高镁安山岩-埃达克质安山岩-富Nb玄武岩组合,伴随俯冲作用的进行,也会形成一些重要的铜金矿床;在太平洋西岸,无震海岭或大洋高原大多发生了较高角度(>30°)的俯冲,且形成了较大规模的玄武岩-玄武安山岩-安山岩组合,其与俯冲流体交代地幔楔熔融产生的岩浆经过分离结晶有关.日本西南部有残佘弧脊发生了俯冲,产生了玄武岩、高镁安山岩和埃达克岩,同时有金矿伴生.除了岩浆作用和铜金成矿之外,脊或海岭的俯冲也可能会导致俯冲带俯冲侵蚀作用发生.需要进一步关注的前沿领域包括脊或海岭俯冲的形式及其动力学机制与物质循环过程、岩浆和金属作用产生的深部机制及影响因素、前新生代的脊或海岭俯冲作用的识别以及板块构造启动时间与太古代大陆地壳生长机制等. | 王强 唐功建 郝露露 Derek WYMAN 马林 但卫 张修政 刘金恒 黄彤宇 许传兵 | 2020 | 中国科学:地球科学2020，50，10： | 5 |
| 7 | Ridge subduction, magmatism, and metallogenesis显示文摘Modern oceans contain large bathymetric highs(spreading oceanic ridges,aseismic ridges or oceanic plateaus and inactive arc ridges)that,in total,constitute more than 20–30%of the total area of the world’s ocean floor.These bathymetric highs may be subducted,and such processes are commonly referred to as ridge subduction.Such ridge subduction events are not only very common and important geodynamic processes in modern oceanic plate tectonics,they also play an important role in the generation of arc magmatism,material recycling,the growth and evolution of continental crust,the deformation and modification of the overlying plates,and metallogenesis at convergent plate boundaries.Therefore,these events have attracted widespread attention.The perpendicular or high-angle subduction of mid-ocean spreading ridges is commonly characterized by the occurrence of a slab window,and the formation of a distinctive adakite–high-Mg andesite–Nb-enriched basalt-oceanic island basalt(OIB)or a mid-oceanic ridge basalt(MORB)-type rock suite,and is closely associated with Au mineralization.Aseismic ridges or oceanic plateaus are traditionally considered to be difficult to subduct,to typically collide with arcs or continents or to induce flat subduction(low angle of less than 10°)due to the thickness of their underlying normal oceanic crust(>6–7 km)and high topography.However,the subduction of aseismic ridges and oceanic plateaus occurred on both the western and eastern sides of the Pacific Ocean during the Cenozoic.On the eastern side of the Pacific Ocean,aseismic ridges or oceanic plateaus are being subducted flatly or at low angles beneath South and Central American continents,which may cause a magmatic gap.But slab melting can occur and adakites,or an adakite–high-Mg andesite–adakitic andesite–Nb-enriched basalt suite may be formed during the slab rollback or tearing.Cu-Au mineralization is commonly associated with such flat subduction events.On the western side of the Pacific Ocean,however,aseismic ridges and oceanic plateaus are subducted at relatively high angles(>30°).These subduction processes can generate large scale eruptions of basalts,basaltic andesites and andesites,which may be derived from fractional crystallization of magmas originating from the subduction zone fluid-metasomatized mantle wedge.In addition,some inactive arc ridges are subducted beneath Southwest Japan,and these subduction processes are commonly associated with the production of basalts,high-Mg andesites and adakites and Au mineralization.Besides magmatism and Cu-Au mineralization,ridge subduction may also trigger subduction erosion in subduction zones.Future frontiers of research will include characterizing the spatial and temporal patterns of ridge subduction events,clarifying the associated geodynamic mechanisms,quantifying subduction zone material recycling,establishing the associated deep crustal and mantle events that generate or influence magmatism and Cu-Au mineralization,establishing criteria to recognize pre-Cenozoic ridge subduction,the onset of modernstyle plate tectonics and the growth mechanisms for Archean continental crust. | Qiang WANG Gongjian TANG Lulu HAO Derek WYMAN Lin MA Wei DAN Xiuzheng ZHANG Jinheng LIU Tongyu HUANG Chuanbing XU | 2020 | Science China Earth Sciences2020，63，10： | 3 |
| 8 | What makes a cry a cry? A review of infant distress vocalizations显示文摘 | Susan LINGLE Megan T. WYMAN Radim KOTRBA Lisa J. TEICHROEB Cora A. ROMANOW | 2012 | Current Zoology2012，58，5： | 2 |
| 9 | Guidelines for the Echocardiographic Assessment of the Right Heart in Adults: A Report from the American Society of Echocardiography显示文摘 | Lawrence G. Rudski Wyman W. Lai Jonathan Afilalo Lanqi Hua Mark D. Handschumacher Krishnaswamy Chandrasekaran Scott D. Solomon Eric K. Louie Nelson B. Schiller | 2010 | Journal of the American Society of Echocardiography2010，，7： | 2 |
| 10 | Do cratons preserve evidence of stagnant lid tectonics?显示文摘Evidence for episodic crustal growth extending back to the Hadean has recently prompted a number of numerically based geodynamic models that incorporate cyclic changes from stagnant lid to mobile lid tectonics. A large part of the geologic record is missing for the times at which several of these cycles are inferred to have taken place. The cratons, however, are likely to retain important clues relating to similar cycles developed in the Mesoarchean and Neoarchean. Widespread acceptance of a form of plate tectonics by ~3.2 Ga is not at odds with the sporadic occurrence of stagnant lid tectonics after this time. The concept of scale as applied to cratons, mantle plumes and Neoarchean volcanic arcs are likely to provide important constraints on future models of Earth's geodynamic evolution. The Superior Province will provide some of the most concrete evidence in this regard given that its constituent blocks may have been locked into a stagnant lid relatively soon after their formation and then assembled in the next global plate tectonic interval. Perceived complexities associated with inferred mantle plume — volcanic arc associations in the Superior Province and other cratons may be related to an over estimation of plume size. A possible stagnant lid episode between ~2.9 Ga and ~2.8 Ga is identified by previously unexplained lapses in volcanism on cratons, including the Kaapvaal, Yilgarn and Superior Province cratons. If real, then mantle dynamics associated with this episode likely eliminated any contemporaneous mantle plume incubation sites, which has important implications for widespread plumes developed at ~2.7 Ga and favours a shallow mantle source in the transition zone. The Superior Province provides a uniquely preserved local proxy for this global event and could serve as the basis for detailed numerical models in the future. | Derek Wyman | 2018 | Geoscience Frontiers2018，9，1： | 2 |
| 11 | Self-assembly and chemical processing of block copolymers:A roadmap towards a diverse array of block copolymer nanostructures显示文摘Block copolymers can yield a diverse array of nanostructures.Their assembly structures are influenced by their inherent structures,and the wide variety of structures that can be prepared especially becomes apparent when one considers the number of routes available to prepare block copolymer assemblies.Some examples include self-assembly,directed assembly,coupling,as well as hierarchical assembly,which can yield assemblies having even higher structural order.These assembly routes can also be complemented by processing techniques such as selective crosslinking and etching,the former technique leading to permanent structures,the latter towards sculpted and the combination of the two towards permanent sculpted structures.The combination of these pathways provides extremely versatile routes towards an exciting variety of architectures.This review will attempt to highlight destinations reached by LIU Guojun and coworkers following these pathways. | WYMAN Ian LIU GuoJun | 2013 | Science China Chemistry2013，56，8： | 2 |
| 12 | Features of promising technologies for pretreatment of lignocellulosic biomass显示文摘 | MOSIER N WYMAN C DALE B | 2005 | Bioresource Technology2005，96，： | 1 |
| 13 | Microsatellite analysis of genetic diversity in four populations of Populus tremuloids in Quebec显示文摘 | Wyman J Bruneau A Tremblay M F | 2003 | Can J Bot2003，81，： | 1 |
| 14 | Combined sugar yields for dilute sulfuric acid pretreatment of corn stover followed by enzymatic hydrolysis of the remaining solids显示文摘 | Lloyd T A Wyman CE | 2005 | Bioresour Technol2005，96，18： | 1 |
| 15 | Likely features and costs of mature biomass ethanol technology显示文摘 | Lynd L R Elander R T Wyman C E | 1996 | Applied biochemistry and biotechnology1996，5758，1： | 1 |
| 16 | Absence of mutagenic activity of sodium borate (borax)and boric acid in the Salmonella preincubation test 显示文摘 | Benson WH Birge WJ Wyman DH | 1984 | Environmental Toxicology and Chemistry1984，3，： | 1 |
| 17 | Regulation in Macromolecules, as Illustrated by Hemoglobin 显示文摘 | Wyman J | 1968 | Quart Rev Biophys1968，1，： | 1 |
| 18 | The Death Penalty and Cultural Relativism in International Law 显示文摘 | Wyman James H | 1997 | Journal of Transnational Law & Policy1997，，2： | 1 |
| 19 | Dynamic location : an iconicmodel to synchronize temporal and spatial transportationdata 显示文摘 | Sutton J C Wyman M M | 2000 | Transportation Research Part C2000，，8： | 1 |
| 20 | Interaction of hemojuvelin- with neogenin results in iron accumulation in human embryonic kidney 293 cells显示文摘 | Zhang AS West AP Jr Wyman AE | 2005 | JBiolChem2005，280，33： | 1 |
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