|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Metamorphic Characteristics and Tectonic Implications of the Kadui Blueschist in the Central Yarlung Zangbo Suture Zone,Southern Tibet显示文摘The Kadui blueschist is located in the central section of Yarlung Zangbo suture zone(YZSZ), southern Tibet, and has been subjected to the subduction of the Neo-Tethyan Ocean below the Asian Plate and provides important clues for better understanding the evolution of the India-Asia convergence zone. In this paper, the systematical petrographic and mineral chemical studies were carried out on the Kadui blueschist, which reveal a mineral assemblage of sodic amphibole, chlorite, epidote, albite and quartz with accessory minerals of titanite, calcite and zircon. Electron microprobe analyses demonstrate that amphibole shows zoned from actinolite core to ferrowinchite/riebeckite rim composition indicating that the sodic amphibole has formed during a prograde metamorphic event. The protolith of the blueschist is an intermediate-basic pyroclastic rock. The calculated pseudosection indicates a clockwise P-T path and constrains peak metamorphic conditions of about 5.9 kbar at 345 ℃. This condition is transitional between pumpellyite-actinolite, greenschist and blueschist facies with a burial depth of 20–22 km and a thermal gradient of 15–16 ℃/km. This thermal gradient belongs to high pressure intermediate P/T facies series and is possibly related to a warm subduction setting of young oceanic slabs. Our new findings indicate that the Kadui blueschist in the central part of YZSZ experienced a rapid subduction and exhumation process as a response to a northward subduction of the Neo-Tethyan oceanic lithosphere during the initial India-Asia collision stage. | Guangming Sun Xu-Ping Li WenYong Duan Shuang Chen Zeli Wang Lingquan Zhao Qingda Feng | 2018 | Journal of Earth Science2018，29，5： | 12 |
| 2 | Optimal Planning of Charging Station for Electric Vehicle Based on Quantum PSO Algorithm显示文摘 | LIU Zifa ZHANG Wei WANG Zeli | 2012 | 中国电机工程学报2012，32，22： | 9 |
| 3 | Crystal structure of PHD domain of UHRF1 and insights into recognition of unmodified histone H3 arginine residue 2显示文摘 | LuluHu ZeLi PingWang YanLin YanhuiXu | 2011 | Cell Research2011，21，9： | 7 |
| 4 | Metamorphic Petrology of Clinopyroxene Amphibolite from the Xigaze Ophiolite,Southern Tibet: P-T Constraints and Phase Equilibrium Modeling显示文摘The clinopyroxene amphibolite from the Bailang terrane is located in the central section of the Yarlung Zangbo suture zone(YZSZ),southern Tibet.The study of it is expected to provide important clues for the subduction of the Neo-Tethyan Ocean below the Asian Plate and thus for better understanding of the development of the India-Asia collision zone.Based on integrated textural,mineral compositional,metamorphic reaction history and geothermobarometric studies of the clinopyroxene amphibolite within a serpentinite mélange,four overprinted metamorphic stages are established.They are the first metamorphic record of M1 stage indicated by a relict assemblage of plagioclase+clinopyroxene+amphibole,an early M2 stage characterized by an assemblage of medium-grained clinopyroxene+amphibole+plagioclase+quartz as well as rutile inclusion in titanite,which is formed during burial process,an isobaric cooling M3 stage which is characterized by an assemblage of clinopyroxene+amphibole+plagioclase+titanite,and a decomposing retrograde stage M4,which is represented by the amphibolite+plagioclase symplectite+titanite+rutile+quartz.By applying the THERMOCALC(versions 6.2 and 6.3)technique in the NCFMASHTO system,the P-T conditions estimated from M1 to M4 stages are ca.8.6 kbar/880℃,10.8–13.4 kbar/800–840℃,12.7–13.2 kbar/650–660℃ and<11.2 kbar/640℃,respectively.The mineral assemblages and their P-T conditions define a counterclockwise P-T path for the clinopyroxene amphibolite of the Xigaze ophiolite,suggesting that the rocks underwent a cooling process during burial from magmatic protolith,and a decompressing stage after the pressure peak metamorphic conditions,which implies that the Bailang terrane of the Xigaze ophiolite may have experienced subduction/collision-related tectonic processes.The peak metamorphism reaches to the transitional P-T conditions among amphibolite facies,granulite facies and eclogite facies with a burial depth of 30–40 km.After exhumation of the ophiolitic unit to the shallow crustal levels,the clinopyroxene amphibolite exposes to a high fO2 condition on the basis of the stable epidotebearing assemblage in the T-MO2 diagrams.A late subgreenschist facies overprinting subsequently occurs,the relevant mineral assemblage is prehnite+albite+chlorite+epidote+quartz. | Yancheng Zhang Xu-Ping Li Guangming Sun Zeli Wang Wenyong Duan | 2019 | Journal of Earth Science2019，30，3： | 7 |
| 5 | Regulation of Leaf Angle by Auricle Development n Maize显示文摘 | Fanying Kong Tingting Zhang Jisheng Liu Siqi Heng Qingbiao Shi Haisen Zhang Zeli Wang Lei Ge Pinghua Li Xiaoduo Lu Gang Li | 2017 | Molecular Plant2017，10，3： | 5 |
| 6 | Redefinition and Formation Age of the Tanjianshan Group in Xitieshan Region, Qinghai显示文摘The Tanjianshan Group, which was previously divided into a, b, c and d formations, has been controversial for a long time. It mainly distributes in the northern margin of Qaidam Basin and is an important early Paleozoic greenschist facies metamorphic volcanic sedimentary rock formation. Detailed field investigation and zircon LA-ICPMS U-Pb dating of the key strata suggest that the original lower part of a Formation(a-1) versus the original middle upper of d Formation(d-3 and d-4), the original upper part of a Formation(a-2) and b Formation versus the original lower part of d Formation(d-1 and d-2) of Tanjianshan Group are contemporaneous heterotopic facies volcanicclasolite deposit, respectively. The former formations formed during the middle-late Ordovician(463–458 Ma), while the latter ones formed in the late Ordovician(about 445 Ma). The original c formation of Tanjianshan Group, which formed after 430 Ma, is similar to the Maoniushan Formation of Kunlun Mountains and north Qaidam Basin. According to the rules of stratigraphic division and naming, new stratum formations of Tanjianshan Group are re-built and divided into Duancenggou(O1-2td), Zhongjiangou(O2-3tz) and Xitieshan(O3tx) formations. The original c Formation is separated from Tanjianshan Group and is renamed as the Wuminggou Formation(S3-D1w), which shows a discordant contact with underlying Tanjianshan Group and overlying Amunike Formation(D3a). The zircon U-Pb age frequency spectrogram of Tanjianshan Group indicates three prominent peaks of 430 Ma, 460 Ma and 908 Ma, which is consistent with the metamorphic and magmatic crystallization ages obtained from para- and orthogneisses in north Qaidam HP-UHP metamorphic belt, implying that strong Caledonian and Jinningian tectonic and magmatic events have ever happened in North Qaidam. | LIANG Xinquan FU Jiangang WANG Ce JIANG Ying ZHOU Yun YANG Yongqiang WANG Zeli PAN Chuanchu | 2014 | Acta Geologica Sinica(English Edition)2014，88，2： | 3 |
| 7 | Relationship between space charge and nonlinear characteristics of ZnO varistor显示文摘In order to reveal the conduction mechanism of ZnO varistor, the pulsed electroacoustic (PEA) measurement is employed to investigate the space charge distribution characteristics of ZnO varistors under different current densities in this paper. Experimental results show that the relationship between the space charge and the current density is consistent with the voltage-current characteristics, and can reflect the nonlinear characteristics of ZnO varistor. The space charge increases linearly with the increase of the electric field strength and the current density in the small current region, this reflects the decrease of the surface states of the grain boundary and changes of the Schottky barrier. There exists a transition region between the small current and middle current regions, where the current is composed of the current by the emission of thermally activated electrons and the tunneling current. In the middle current region, the space charge will decrease as the current increases, and will disappear with the depletion layer decreasing to zero. | WANG Qian TU YouPing DING LiJian JU ZeLi | 2011 | Science China(Technological Sciences)2011，54，7： | 2 |
| 8 | Prevale nee and spatial distribution patterns of human echinococcosis at the township level in Sichuan Province, China显示文摘Background:Echinococcosis is a global zoonotic parasitic disease caused by Echinococcus larvae.This disease is highly endemic in Sichuan Province,China.This study investigates the prevalence and spatial distribution characteristics of human echinococcosis at the township level in Sichuan Province,geared towards providing a future reference for the development of precise prevention and control strategies. | Wei He Li-Ying Wang Wen-Jie Yu Guang-Jia Zhang Bo Zhong Sha Liao Qi Wang Rui-Rui Li Liu Yang Ren-Xin Yao Yang Liu Zeli Dan ba Sheng-Chao Qin Shi-An Wang Yan-Xia Wang Yan Huang Qian Wang | 2021 | Infectious Diseases of Poverty2021，10，3： | 2 |
| 9 | Removal of trace and major metals by soil washing with Na2EDTA and oxalate显示文摘 | Rongliang Qiu Zeli Zou Zhihao Zhao Weihua Zhang Tao Zhang Hanying Dong Xiange Wei | 2010 | Journal of Soils and Sediments2010，，1： | 1 |
| 10 | Outcome evaluation of 10317 laparoseopic cholecystectomies : a 17-year experience at a single center 显示文摘 | Grbas H Kunisek L Zelie M | 2013 | Hepatogastroenterology2013，60，128： | 1 |
| 11 | A mathematical model for predic- tion of compressive strength in cement-silica fume blends 显示文摘 | Zeli J Rui D Krstulovi R | 2004 | Cement and Concrete Research2004，34，12： | 1 |
| 12 | Combined multi-direct forcing and immersed boundary method for simulating flows with moving particles 显示文摘 | Wang Zeli Fan Jianren Luo Kun | 2008 | International Journal of Multiphase Flow2008，34，3： | 1 |
| 13 | Intravenous labetalol in acute aortic dissection显示文摘 | Grubb BP Zelis CR | 1987 | JAMA1987，258，1： | 1 |
| 14 | Formaldehyde emission from wood products: relationship between the values by the Chamber method and those by the Desiccator test显示文摘 | Zeli Que Takeshi Furuno | | 0，，： | 1 |
| 15 | Immersed boundary method for the simulation of flows with heat transfer显示文摘 | Wang Zeli Fan Jianren Luo Kun | 2009 | International Journal of Heat and Mass Transfer2009，52，1920： | 1 |
| 16 | Regulation of tissue noradrenaline in the rat myocardial infarction model of chronic heart failure显示文摘 | Clemson B Baily R | 1992 | Cardiovasc Res1992，26，10： | 1 |
| 17 | Strength and stability of frictional sliding of gabbro gouge at elevated tempera- tures 显示文摘 | He Changrong Yao Wenming Wang Zeli | 2006 | Tectonophysics2006，427，1： | 1 |
| 18 | Effects of urea-formaldehyde resin mole ration on the properties of particleboard显示文摘 | Zeli Que Takeshi Furuno Sadanobu Katoh | 2007 | Building and Environment2007，42，： | 1 |
| 19 | Frictional sliding of gabbro gouge under hydrothermal conditions 显示文摘 | He Changrong Wang Zeli Yao Wenming | 2007 | Tectonophysics2007，445，3： | 1 |
| 20 | Thermodynamics of reactions of CIHg and BrHg radicals with atmospherically abundant free radicals 显示文摘 | Dibble T S Zelie M J Man H | 2012 | Atmospheric Chemistry and Physics2012，12，10： | 1 |
您所在的机构暂未开通此部分的功能，请联系管理员