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13篇 您的检索式:作者名="SUNYan"
    题名 作者 年代 出处 被引量
1Observation of ultra-microtexture of fault rocks in shearing-sliding zones显示文摘Based on scanning electronic microscopic observation of three fault rocks in ductile-brittle shearing-sliding zones (including one palimpsest mylonite sampled from deep bore cores of Cajon Pass, California, two flowing-structured carbargillites sampled from Shaancan Well 1 located in north Shaanxi, and Well NH located in Huanghai, respectively), micron- and nanometer-scaled ultra-fine grinding grain texture of fault rocks is discovered in this study. And the geological significance of grinding grain texture is discussed in terms of its particulate organization, rheology of particulate slipping, laminar petrography and micro dynamics including dynamothermal metamorphism, fluid transferring, particulate autorotation, and so on. In addition, the remaining problems to be solved and broad prospects in this new study field are also discussed.SUNYan LUXiancai SHULiangshu GULianxing ZHUWenbin GUOJichun LINAiming 2005Progress in Natural Science:Materials International2005,15,5:8
2Mesozoic-Cenozoic thermal history of Turpan-Hami Basin: apatite fission track constraints显示文摘Apatite fission track dating is carried out on nine samples collected from the central part (Lianmuqin section) and from both northern and southern margins of Turpan Hami Basin. The fission track ages of seven Jurassic samples are distinctly younger than depositional ages. In contrast, the fission track ages of two Cretaceous samples are older than, or as old as depositional ages. These observations indicate that the Jurassic samples have been annealed or partially annealed, whereas the Cretaceous samples have not been annealed. The further thermal modelling results show that Turpan Hami Basin experienced a Late Cretaceous period (120-100 Ma) of tectonic uplift with rapid cooling and exhumation of sediments. The samples underwent a Cenozoic period of reburial and re heating and were exhumed again at 10-8 Ma.ZHUWenbin WANJinglin SHULiangshu SUNYan GUOJichun WANGFeng 2005Progress in Natural Science:Materials International2005,15,4:7
3Preparation and Visible-light Photochromism of Phosphomolybdic Acid/Polyvinylpyrrolidone Hybrid Film显示文摘SUNYan WANGXiansheng LUYamei XUANLimin XIAShuang FENGWei HANXiangkui 2014Chemical Research in Chinese Universities2014,30,5:5
4Prospects for study of tectono-geochemistry显示文摘Focusing on fault tectono-geochemistry, the authors will illustrate four aspects of the fault tectono-geochemistry and its research prospects: (1) the major elements, trace elements and rare earth elements and their differentiation and dissipation sequence; (2)mineral veins, secondary inclusions, sync-deformation fluids and their micro-kinetic analyses; (3) pressure intensity, temperature grads,solution concentration and their coupled correlation system; (4) tectonic stress fields, rheologic physical fields, geochemical fields and digital modeling of parameters. The four aspects are unique in their own systems and related to one another. A unified explanation of spatial and temporal evolution can be obtained in combination with the geodynamics and tectonic chronology.ZHUWenbin SunYan GUOJichun LIUDeliang AimingLIN 2003Progress in Natural Science:Materials International2003,13,3:2
5Tectono-geochemistry analyses of fault rocks in shear zone of metamorphic core complex in north Jiangxi, China显示文摘Through a systematic sampling test and mass equilibrium analysis of the three sorts of complex assemblages (intrusive complex, tectonic complex and metamorphic complex) penetrating the metamorphic core complex (MCC) in the Xingzi area of north Jiangxi, the authors find that, like major elements, the trace elements of small ion radius, big specific gravity and high potential form the accumulative series in fault rocks, instead of divergence series. In rare earth elements, ΣREE and HREE are relatively centralized, characteristic of rising and Eu loss in the distribution pattern. Only on the upside of the ductile fault, there exist some phenomena contrary to the general rules, most of which are restricted by the rock rheologic differentiation, coupling of mechanics and chemistry, and inversion of tectonic regime.SUNYan SHULiangshu GUOJichun ZHUWenbin ZHANGXihui CHENXiangyun WANGFeng FAUREM 2003Progress in Natural Science:Materials International2003,13,5:2
6Study and implementation on the grey comprehensive evaluation support system of eco-city显示文摘HUANG Kun CHEN Senfa SUNYan 2002Journal of Southest University2002,18,4:1
7显示文摘XUBin-He(徐兵河) SUNYan(孙燕) ZhongguoXinyaoZazhi0,,:1
8显示文摘WANGWei(王伟) WANGJing(王静) YANGCai-qin(杨彩琴) SUNYan(孙严) LVYa-qi(吕雅琪) DONGLi-long(董立龙) 2012理化检验:化学分册2012,48,7:1
9TiO2 nanotubesforhydrogengenerationbyphotocatalyticwatersplittinginatwo-compartmentphotoelectrochemicalcell显示文摘SunYan WangGuixin YanKangping 2011InternationalJournalofHydrogenEnergy2011,36,15:1
10A Study on Arylesterase's Substrate,Method and Clinical Application显示文摘HUWang-Ping ZHOUChang-Shao HUYing-Ying SUNYan 2003生物化学与生物物理学报2003,35,11:0
11Determination of Serum Bilirubin with The Periodate Oxidation Method显示文摘HUWang-Ping HUYing-Ying SUNYan ZHENGWei-Qiang 2003生物化学与生物物理学报2003,35,11:0
12Steel Tower Design for 500 kV Power Line in Indonesia显示文摘This paper briefly introduces the designand test of steel towers for 500 kV power linein Indonesia by our Institute. It specifiesdesign criteria, tower configurationarrangement and constitution, calculationand analysis of steel towers and the tests onthree prototypes. Experience obtained fromthis work, together with some opinions on theapplication of American 'Guide for Designof Steel Transmission Towers', is presented.Wei Sunyan Yang Yuanchun 1997Electricity1997,,4:0
13ON THE EXISTENCE OF POSITIVE SOLUTIONS FOR SINGULAR NEUMANN BOUNDARY VALUE PROBLEMS显示文摘By using fixed point index theory, we consider the existence of positive solutions for singular nonlinear Neumann boundary value problems. Our main results extend and improve many known results even for non-singular cases.SunYan XuBenlong SunYongping 2005Annals of Differential Equations2005,21,2:0
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