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| 1 | History and possible mechanisms of prehistoric human migration to the Tibetan Plateau显示文摘Prehistoric human history on the Tibetan Plateau is a hotly debated topic. Archaeological research on the plateau during the past few decades has enormously improved our understanding of the topic and makes it possible for us to consider the processes and mechanisms of prehistoric human migration to the region. By reviewing the published archaeological research on the Tibetan Plateau, we propose that the first people on the plateau initially spread into the He-Huang region from the Chinese Loess Plateau, and then moved to the low elevation Northeastern Tibetan Plateau and perhaps subsequently to the entire plateau. This process consisted of four stages.(1) During the climatic amelioration of the Last Deglacial period(15–11.6 ka BP), Upper Paleolithic hunter-gatherers with a developed microlithic technology first spread into the Northeastern Tibetan Plateau.(2) In the early-mid Holocene(11.6–6 ka BP), Epipaleolithic microlithic hunter-gatherers were widely distributed on the northeastern plateau and spread southwards to the interior plateau, possibly with millet agriculture developed in the neighboring low elevation regions.(3) In the mid-late Holocene(6–4 ka BP), Neolithic millet farmers spread into low elevation river valleys in the northeastern and southeastern plateau areas.(4) In the late Holocene(4–2.3 ka BP), Bronze Age barley and wheat farmers further settled on the high elevation regions of the Tibetan Plateau, especially after 3.6 ka BP. Finally, we suggest that all of the reported Paleolithic sites earlier than the LGM on the Tibetan Plateau need further examination. | ZHANG DongJu DONG GuangHui WANG Hui REN XiaoYan HA PiPu'u QIANG MingRui CHEN FaHui | 2016 | Science China Earth Sciences2016，59，9： | 20 |
| 2 | Origin of Listwanite in the Luobusa Ophiolite,Tibet,Implications for Chromite Stability in Hydrothermal Systems显示文摘Listwanite from the Luobusa ophiolite,Tibet,forms a narrow,discontinuous band along the eastern part of the southern boundary fault. We undertook a detailed petrographic and geochemical study to understand the mineral transformation processes and the behaviour of major and trace elements during listwanite formation. Three alteration zones characterized by distinct mineral components and texture are recognized and,in order of increasing degree of alteration,these are: zoneIII is rich in serpentine minerals; zoneII is rich in talc and carbonates; and zoneI is mainly composed of carbonates and quartz. Geochemical data for the three alteration zones show significant modification of some major and trace elements in the protolith,although some oxides show linear correlations with Mg O. Gold mineralization is recognized in the Luobusa listwanite and may signify an important target for future mineral exploration. Gold enrichment occurs in both zoneI and zoneIIand is up to 0.91 g/t in one sample from zoneI. We show that CO2-rich hydrothermal fluids can modify both the occurrence and composition of chromite grains,indicating some degree of chromite mobility. Low-Cr anhedral grains are more easily altered than high-Cr varieties. The compositions of chromite and olivine grains in the listwanite suggest a dunite protolith. | ZHANG Lan YANG Jingsui Paul T.ROBINSON XIONG Fahui CHEN Yanhong LAI Shengmin CHEN Mei | 2015 | Acta Geologica Sinica(English Edition)2015，89，2： | 6 |
| 3 | Geochronology and Geochemistry of the Subduction-related Rocks with High Sr/Y Ratios in the Zedong Area: Implications for the Magmatism in Southern Lhasa Terrane during Late Cretaceous显示文摘南部的拉萨岩层以它在中生代和新生代期间记录 magmatism 的巨大的 magmatic 带著名。尽管在南部的拉萨岩层的中生代大陆人边缘背景被识别了,在迟了的白垩纪期间的这构造设定和进化历史的细节仍然保持不清楚。为了推进,抑制这些问题,我们现在的锆石 LA-ICP-MS U-Pb,同位素的 Hf 和 Sangri 的 Gongbari dacites 的 geochemical 数据组织哪个从南部的拉萨岩层的东方部分由古新的 granodiorites 侵入了,西藏。新年龄数据显示 dacites 在 ∼95.4 妈被产生,它建议 Sangri 组火山作用可以持续到迟了的白垩纪。Gongbari dacites 被高 Sr 428-758 ppm 内容描绘,例如 Yb=0.78-1.14 ppm 的重稀土元素元素和 Y 的低集中;有高 Sr/Y 41.91-67.59 和 La/Yb 22.64-30.64 比率的 Y=8.85-11.4 ppm,类似于那些 adakite。岩石是计算碱的, metaluminous,在 LILE 充实,在 HFSE 弄空,并且有积极 ε Hf t 价值 +7.7 到 +11.6。Gongbari dacites 被到石榴石角闪岩外形条件的在角闪岩下面的年轻、热的 subducted Neo-Tethyan 海洋的外壳的部分融化可能生产。尽管 Gangdese 山可能形成了以前 Indo 亚洲的碰撞,拉萨岩层的南部的边缘可能不通过显然外壳的变厚在期间向北方 Neo-Tethyan 的 subduction 海洋的岩石圈。 | CHEN Yanhong YANG Jingsui XIONG Fahui ZHANG Lan LAI Shengmin CHEN Mei | 2015 | Acta Geologica Sinica(English Edition)2015，89，2： | 6 |
| 4 | Petrological and Os Isotopic Characteristics of Zedong Peridotites in the Eastern Yarlung–Zangbo Suture in Tibet显示文摘The Zedong ophiolites in the eastern Yarlung–Zangbo suture zone of Tibet represent a mantle slice of more than 45 km^2. This massif consists mainly of mantle peridotites, with lesser gabbros, diabases and volcanic rocks. The mantle peridotites are mostly harzburgite, lherzolite; a few dike-like bodies of dunite are also present. Mineral structures show that the peridotites experienced plastic deformation and partial melting. Olivine(Fo89.7–91.2), orthopyroxene(En_(88–92)), clinopyroxene(En_(45–49) Wo_(47–51) Fs_(2–4)) and spinel [Mg~#=100×Mg/(Mg+Fe)]=49.1–70.7; Cr~#=(100×Cr/(Cr+Al)=18.8–76.5] are the major minerals. The degree of partial melting of mantle peridotites is 10%–40%, indicating that the Zedong mantle peridotites may experience a multi–stage process. The peridotites are characterized by depleted major element compositions and low REE content(0.08–0.62 ppm). Their 'spoon–shaped' primitive–mantle normalized REE patterns with(La/Sm)_N being 0.50–6.00 indicate that the Zedong ultramafic rocks belong to depleted residual mantle rocks. The PGE content of Zedong peridotites(18.19–50.74 ppb) is similar with primary mantle with Pd/Ir being 0.54–0.60 and Pt/Pd being 1.09–1.66. The Zedong peridotites have variable, unradiogenic Os isotopic compositions with ^(187)Os/^(188)Os=0.1228 to 0.1282. A corollary to this interpretation is that the convecting upper mantle is heterogeneous in Os isotopes. All data of the Zedong peridotites suggest that they formed originally at a mid-ocean ridge(MOR) and were later modified in supra–subduction zone(SSZ) environment. | LAI Shengmin YANG Jingsui Yildirim DILEK XIONG Fahui JIANG Rui CHEN Yanhong | 2018 | Acta Geologica Sinica(English Edition)2018，92，2： | 2 |
| 5 | Location analysis of retail stores in Changchun, China: A street centrality perspective显示文摘 | Fahui Wang Chen Chen Chunliang Xiu Pingyu Zhang | 2014 | Cities2014，，： | 1 |
| 6 | Location analysis of retail stores in Changchun, China: A street centrality perspective显示文摘 | Fahui Wang Chen Chen Chunliang Xiu Pingyu Zhang | 2014 | Cities2014，，： | 1 |
| 7 | Effect of heat treatment on the potential allergenicity and conformational structure of egg allergen ovotransferrin显示文摘 | Ping Tong Jinyan Gao Hongbing Chen Xin Li Yin Zhang Shan Jian Harry Wichers Zhihua Wu Anshu Yang Fahui Liu | 2011 | Food Chemistry2011，，2： | 1 |
| 8 | Structure tailorable triple-phase and pure double-polar-phase flexible IF-WS_(2)@poly(vinylidene fluoride)nanocomposites with enhanced electrical and mechanical properties显示文摘A new low-cost high-permittivity flexible nanocomposite consisting of a polyvinylidene fluoride(PVDF)matrix and fullerene-like tungsten disulfide nanoparticle(IF-WS2 NP)filler was fabricated via a simple solution route.A comprehensive investigation by X-ray diffraction,attenuated total reflection-infrared spectroscopy,and differential scanning calorimetry(DSC)showed that 0.5e1 vol% of IF-WS_(2) induced a nonpolar α-phase to coexisting triple-phase transition in PVDF,whereas a slightly higher loading of 2 vol% induced pure double-polar β- and γ-phases.These results indicate that the structure and properties of the fabricated nanocomposite are easily tailorable.DSC during heating and cooling cycles and morphology observations further indicated that a polar phase was induced by the nucleation effect of the IF-WS2 NPs and electrostatic interactions.As a consequence of the multiphase coexistence and structure homogeneity,nanocomposites with approximately 0.5-1 vol% of IF-WS_(2) NPs showed enhanced dielectric and energy-storage performance as well as enhanced tensile strength and elongation.The new phase-tailorable nanocomposites with balanced properties are promising for applications as energystorage capacitors,piezoelectric sensors,and other flexible multifunctional components.The results of this study will serve to deepen the understanding of the polymer polymorph and provide directions on new routes for fabrication of smart materials. | Dong Guo Kai Cai Pingye Deng Guoning Si Liangying Sun Fahui Chen Honglong Ning Li Jin Jingtao Ma | 2020 | Journal of Materiomics2020，6，3： | 0 |
| 9 | Geochronology and Geochemistry of the Magmatic Rocks from Zedong Ophiolite, Eastern Yarlung-Zangbo Suture Zone, Tibet显示文摘The Yarlung Zangbo suture zone extends more than2000 km along southern Tibet and marks the boundary between the Indian subcontinent and Eurasia.The Zedong terrane has been not suggested to represent the vestige of such an intra-oceanic arc developed within the Neo-Tethys Ocean,as a result of the northward subduction of the Neo-Tethys Ocean during the Late Jurassic.In this study,we present detailed geochemical and geochronological data of various types of magmatic rocks widely exposed in the Zedong terrane to constrain the formation age and tectonic setting of the Zedong terrane.We found that the Zedong volcanic rocks belong to high K2O calc-alkaline series,whereas the diabase and gabbro plotted in the low-K calcalkline.The basalt rocks are highly enriched in LREE and LILE,but strongly depleted in HFSE,indicating they were derived from a metasomatized mantle.Both gabbros and diabase have similar N-MORB geochemistry indicates that the cumulates were produced from MOR setting.Zircons from four samples,including the basalt rocks(158-161Ma)are older than the gabbro(131 Ma),certificate the gabbro are as the vein intrude into the basalt rocks.This suggests that the volcanic eruption and plutonic emplacement were coevally developed in the Zedonghave similar positiveεHf(t)values(+2.0 to+15.6)and(+8.6 to+18.4),indicating they were stemmed from similarly depleted mantle sources,same with the gabbro and granitic rocks from the Gangdese arc.Therefore,we proposed that the basalt rocks in the Zedong terrane were formed through partial melting of the mantle wedge metasomatized by slab-released fluids/melts.A part of hydrous basalts were underplated in the thickened lower crust beneath the Zedong terrane,which gave rise to the cumulate and granitic rocks.This suggests that the Zedong terrane represents a slice of the active continental margin developed on the southern margin of the Lhasa terrane as a result of the northward subduction of the Neo-Tethys Ocean during the Late Jurassic,although a possible intra-oceanic arc setting cannot be excluded. | XIONG Fahui YANG Jingsui Paul T.ROBINSON GAO Jian ZHANG Lan CHEN Yanhong LAI Shengming | 2017 | Acta Geologica Sinica(English Edition)2017，91，S1： | 0 |
| 10 | The Origins of Zedang Peridotite in Eastern Yarlung-Zangbo Suture in Tibet显示文摘The Zedang mafic-ultramafic body crops out in the eastern Yarlung-Zangbo suture zone of Tibet.This massif consists of mantle peridotite,gabbro,diabase and volcanic rocks.The mantle peridotites are mostly harzburgite,lherzolite and a few harzburgites with chromitite.Dikelike bodies of dunite are also present.Mineral | LAI Shengmin YANG Jingsui XIONG Fahui LIUZhao TIAN Yazhou Xu Xiangzhen ZHANG Lan CHEN Yanhong GAO Jian | 2015 | Acta Geologica Sinica(English Edition)2015，89，A02： | 0 |
| 11 | Petrology of Cr-rich Podiform Chromitites of Bulqiza, Eastern Ophiolitic Belt, Albania显示文摘The ultramafic massif of Bulqiza,which belongs to the eastern ophiolitic belt of Albania,is a major source of metallurgical chromitite ore.The massif consists of a thick(>4 km)sequence,composed from the base upward of tectonized harzburgite with minor dunite,a transitional zone of dunite,and a magmatic sequence of wehrlite, | XIONG Fahui YANG Jingsui ROBINSON Paul T. DILEK Yildirim MILUSHI Ibrahim XU Xiangzhen ZHANG Zhongming ZHOU Wenda CHEN Yanhong HUANG Zhu LAI Shengming ZHANG Lan | 2015 | Acta Geologica Sinica(English Edition)2015，89，A02： | 0 |
| 12 | Diopside and Magnetite Exsolutions in Olivine from Lower Cr# Dunite in the Dongbo Ophiolite, Southern Tibet显示文摘 | XIONG Fahui YANG Jingsui Robinson T PAUL Dilek YILDIRIM CHEN Yanhong XU Xiangzhen LIU Zhao TIAN Yazhou ZHOU Wenda LAI Shengming ZHANG Lan | 2015 | Acta Geologica Sinica(English Edition)2015，89，A02： | 0 |
| 13 | Petrology of Cr-rich Ophiolitic Chromitites of Bulqiza, Eastern Ophiolitic Belt, Albania显示文摘The ultramafic massif of Bulqiza,which belongs to the eastern ophiolitic belt of Albania,is the most important area for metallurgical chromitite ores.The massif consists of a thick(>4 km)rock sequence,with a generalized profile from the bottom to the top as follows.The | XIONG Fahui YANG Jmgsui Paul T. ROBINSON Yildirim DILEK MILUSHI Ibrahim XU Xiangzhen ZHANG Zhongming ZHOU Wenda CHEN Yanhong HUANG Zhu LAI Shengming ZHANG Lan | 2015 | Acta Geologica Sinica(English Edition)2015，89，A02： | 0 |
| 14 | Petrogenesis of Peridotites from the Purang Ophiolite in Western Part of Yarlung-Zangbo Suture Zone, Southern Tibet显示文摘Peridotites are an important part of ophiolites:they not only record plate tectonic settings and events,but also offer help to interpret the composition of the mantle and the effect of the deep mantle.The Yarlung-Zangbo suture zone extends more than 2000 km along southern Tibet,which is the biggest suture zone in China.The | ZHOU Wenda YANG Jingsui ZHAO Junhong MA Changqian XIONG Fahui XU Xiangzhen CHEN Yanhong TIAN Yazhou | 2015 | Acta Geologica Sinica(English Edition)2015，89，A02： | 0 |
| 15 | Microporous Nitrogen-Rich Polymers via Ullmann Coupling Reaction for Selective Adsorption of C_(2)H_(2) over CH_(4)显示文摘Acetylene purification from methane is challenging in the field of porous organic polymers(POPs).Herein,we have provided one-pot Ullmann coupling reaction to synthesize a series of POPs with rich N-sites,named FJU-POP-n,wherein the low-cost and non-toxic Cu(acac)2 and environmental-friendly glycerol are employed as catalyst and solvent,respectively. | Jitao Huang Qinfang Peng Chulong Liu Yingxiang Ye Liangji Chen Yuanchao Lv Yisi Yang Shimin Chen Fahui Xiang Hao Zhang Zhangjing Zhang Shengchang Xiang | 2023 | Chinese Journal of Chemistry2023，41，5： | 0 |
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