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| 1 | Late Mesozoic basin and range tectonics and related magmatism in Southeast China显示文摘在迟了的中生代中间的 JurassicLate 白垩纪期间,盆和范围 tectonics 和 extensional 的联系 magmatism 代表构造设定在由于和平的板 subduction 的东南的中国是普遍的。盆 tectonics 由 post-orogenic 组成(类型我) 并且 intra 大陆人 extensional 盆(类型 II ) 。类型我盆在山麓和 intraland 发展了在期间对早侏罗记,纹理粗糙的陆上的碎屑状的沉积在被扔晚三叠纪。在 intra 大陆人期间形成的类型 II 盆外壳的变瘦并且被 grabens 和 half-grabens 的发展描绘。Graben 盆主要在中间的侏罗记期间被产生并且与 bimodal 火山作用被联系。在 half-grabens 的沉积与 rhyolitic 凝灰岩和熔岩被设置并且近来是在有优势的年龄的早白垩纪 CretaceousPaleogene 红床。范围由 granitoids 和 bimodal 组成暴烈的岩石, A 类型花岗石和屋顶类型变形核心建筑群。作者分析了 lithological, geochemical 和迟了的中生代火的岩石集合的 geochronological 特征并且在形成华南的盆和范围 tectonics 上建议了一些地球动力学的限制。类似的比较和在东方、西方的岸之间的盆和范围 tectonics 的差别和平被做,并且东南中国块的地球动力学的进化模型在迟了的中生代期间被讨论。学习结果建议华南在合拢的中生代前上开发了的在内的盆和范围岩层系上带子从自从迟了的中生代,西方的和平的板的 subduction 主要抑制的多相的构造进化被导出,在一个背弧 extensional 背景导致各种各样的 magmatism 的形成。它的 geodynamic 机制能在东方岸与盆和范围 tectonics 的作比较和平。在两岸之间的盆和范围 tectonics 的差别和平例如披风羽毛形成, extensional 和火的岩石集合和盆和范围 tectonics 的年龄可伸缩,主要被 Yellowstone 披风羽毛在太平洋的东方岸引起。 | Dezi Wang Liangshu Shu | 2012 | Geoscience Frontiers2012，3，2： | 60 |
| 2 | Primary Sn-rich titianite in the Qitianling granite, Hunan Province, southern China: An important type of tin-bearing mineral and its implications for tin exploration显示文摘The Qitianling calc-alkaline granite in Hunan Province (South China) has attracted much attention since the discovery of the Furong super-large tin deposit. The present study provides new mineralogical data to address their implications for exploration of tin deposits. In the Taoxiwo granite in the southeastern part of the Qitianling granite body, Sn-rich titanite was identified as an important type of Sn-bearing mineral. The titanite commonly occurs with biotite as euhedral crystals, exhibiting typical envelope-like shape and sector-zoning texture. These indicate that the titanite most likely crystallized in the mag-matic stage. Electron-microprobe analyses show that the titanite is enriched in tin up to 1.12 wt% SnO2, with an average of 0.43 wt%. With the crystallization of the granite, primary minerals undertook hydro-thermal alteration by magma-derived fluids. Subsequently, in the hydrothermal stage, the primary Sn-bearing titanite was altered (at least partially), but still preserved its typical envelope-shaped outline. Micro-scale cassiterite is a representative product of such alteration; other secondary minerals include fluorite, ilmenite, Sn-bearing rutile and quartz. Therefore, the titanite, commonly present in the calc- alkaline granites, can be treated as an important Sn-carrying mineral in the Qitianling granite, reflecting the primary magmatic environment with tin enrichment. The hydrothermal alteration of the primary titanite and subsequent crystallization of cassiterite recorded a process of leaching and accumulation of tin in magmatic-hydrothermal evolution of the Snbearing granite. Thus, this titanite has important implications for tin exploration. | XIE Lei WANG RuCheng CHEN Jun ZHU JinChu ZHANG WenLan WANG DeZi YU APeng | 2009 | Chinese Science Bulletin2009，54，5： | 10 |
| 3 | Characteristics of Volcanic Rocks in the Shoshonite Province, Eastern China, and Their Metallogenesis显示文摘The shoshonite province in eastern China is characterized by extensive distribution (ca. 80000 km2) of Late Jurassic-Early Cretaceous (165-100 Ma) shoshonite series with subordinate high-K calc-alkali series. It was formed in a dominantly tensile stress field. In comparison with their analogues in island arcs and active continental margins in other countries, the volcanic rocks in the shoshonite province have their specific characteristics in petrology, mineralogy and geochemistry as well as related mineralization association, which are the comprehensive reflection of the special composition and structure of the mantle and crust of the province and the special Mesozoic regional tectonic setting. | Wang Dezi, Ren Qijiang, Qiu Jiansheng, Chen Kerong,Xu Zhaowen and Zeng Jiahu Department of Earth Sciences, Nanjing University, Nanjing, Jiangsu | 1996 | Acta Geologica Sinica(English Edition)1996，70，3： | 10 |
| 4 | The thermal history of the miarolitic granite at Xincun, Fujian Province, China显示文摘The thermal history of the late Mesozoic miarolitic granite has been studied based on zircon U-Pb dating, whole rock Rb-Sr dating and K-Ar dating of muscovite, biotite and K-feldspar from the same rock sample. From the beginning of zircon crystallization to the closure of K-Ar system of biotite, the granite body had a slow cooling rate (11.0℃/Ma) and an ascending rate (0.07 mm/a). From the end of this stage to the closure of K-Ar system of K-feldspar, the granite body increased its cooling rate (45℃/Ma) and ascending rate (0.36 mm/a). The thermal history of the Xincun granite with a slow cooling rate at the early stage and a fast cooling rate at the late stage may have been related to the fact that the Fujian coastal area had very high geothermal gradient in the late Mesozoic and evident decrease in geothermal gradient in the early Cenozoic. | SHEN Weizhou LING Hongfei LI Huimin LI Wuxian WANG Dezi | 2000 | Chinese Science Bulletin2000，45，21： | 9 |
| 5 | Differentiation and accumulation of fluids in A-type granites: Evidence from accessory mineral study显示文摘The Laoshan A-type granite is a highly evolved granite body. The study on accessoryminerals indicates that there exist differentiation and accumulation of fluids during the late stage of evolution of the granite. The released fluids are rich in rare-earth elements (REE), high-field-strength elements (HFSE, such as Nb, Ta, Zr, Hf, Th, U, and Y) and volatiles (F, P, CO2, etc.). Owing to the presence of fluid, accessory mineral assemblages have changed during the evolution of A-type granite, and are especially characterized by large amounts of independent REE-Nb-Y-Th minerals present in the late facies. Late-accumulation of fluids may be of the general feature of A-type granites, at least of highly evolved ones. | WANG Rucheng ZHAO Guangtao WANG Dezi LU Jianjun XU Shijin | 2000 | Chinese Science Bulletin2000，45，17： | 7 |
| 6 | Yttrium zoning in garnet from the Xihuashan granitic complex and its petrological implications显示文摘The Xihuashan granitic complex is characterized by enrichment in rare-earth elements (REE). In particular, the second-stage granite (G-b) is markedly enriched in yttrium, and therefore contains complex associations of Y-bearing minerals. In this granite, garnet displays specific yttrium zoning with an Y-rich core and a 揷lean?rim. Besides minute inclusions of Y-bearing minerals, garnet involves a striking amount of Y and HREE in its central area. It is suggested that enrichment in Y in the garnet core accords with that in the melt as a result of REE magmatic fractionation. However, the 揷lean?rim may be the direct result of accumulation of fluid phases in the magma, which is virtually unfavorable for the entrance of REE in the garnet structure. | WANG Rucheng, HU Huan, ZHANG Aicheng, XU Shijin & WANG Dezi State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China Correspondance should be addressed to Wang Rucheng (e-mail: rcwang@nju.edu.cn) | 2003 | Chinese Science Bulletin2003，48，15： | 3 |
| 7 | Isotope Geochemical Characteristics and Material Sources of Tin--Bearing Porphyries in South China显示文摘Tin-bearing porphyries in South China can be divided into the F-rich and F-poorsubtypes. They are high-silica (SiO2>71%), peraluminous (A/NKC>1.0) and rich inincompatible elements (Rb, Zr, U, W, Sn) and have weak Ce (δCe=0.68-0.82) and strong Eu(δEu=0.01-0.38) negative anomalies. Meantime, they also have low δNd(-6.3- -8.4), high207Pb/204Pb (15.588-15.790), medium to high (87Sr/86Sr)i (0.7084-0.7287) and relatively highδ18O(9.1-10.3‰). These characteristics clearly suggest that the two subtypes of tin-bearingporphyries were derived from the crustal materials. Their differences lie only in the existence ofcertain different components in their source materials. Therefore, there is only one type oftin-bearing prophyry in South China. that is continental crust transformation type. | Shen Weizhou Wang Dezi and Liu Changshi Department of Earth Sciences, Nanjng University, Nanjng, Jiangsu | 1996 | Acta Geologica Sinica(English Edition)1996，70，2： | 3 |
| 8 | The Mesozoic Volcanic-Intrusive Complexes and the lr Metallogenic Relations in East China 显示文摘 | Wang Dezi Ren Qijiang | 1999 | Beijing:Scicence Press1999，，： | 1 |
| 9 | Nonlinear behavior of externally prestressed composite beam 显示文摘 | Dall Asta A Dezi L | 1998 | Journal of Structural Engineering1998，，5： | 1 |
| 10 | Nonuniform Bending-stress Distribution (Shear Lag) 显示文摘 | Dezi L Mentrasti L | 1985 | Journal of Structural Engineering1985，111，12： | 1 |
| 11 | Discussion on 'prestress force effete on vibration frequency of concrete bridges' 显示文摘 | Dall A A Dezi L St | 1996 | Journal of Structural Engineering1996，122，4： | 1 |
| 12 | Prestress force effect on vibration frequency of concrete bridges discussion 显示文摘 | Dall Asta A Dezi L | 1996 | Journal of Structural Engineering1996，124，4： | 1 |
| 13 | A beam finite element including shear lag effect for the time- dependent analysis of steel-concrete composite decks 显示文摘 | Gara Fabrizio Leoni Graziano Dezi Luigino | 2009 | Engineering Structures2009，31，8： | 1 |
| 14 | Kinematic Bending Moments in Pile Foundations显示文摘 | Dezi F Carbonari S Leoni G | 2010 | Soil Dynamics and Earthquake Engineer-ing2010，30，3： | 1 |
| 15 | Nonlinear Behavior of Externally Prestressed Composite Beams:Analytical Model显示文摘 | Andrea Dall' Asta Luigino Dezi | 1998 | Journal of Structural Engineering1998，，5： | 1 |
| 16 | Nonuniform bending-stress distribution (shear tag) 显示文摘 | Dezi L Mentrasti L | 1985 | Journal of Structural Engineering1985，111，12： | 1 |
| 17 | Prestress force effect on vibration frequency of concrete bridges discussion显示文摘 | Dall Asta A Dezi L | 1996 | Journal of Structural Engineering1996，122，4： | 1 |
| 18 | Algebraic methods for creep analysis of continuous composite beams 显示文摘 | Luigino Dezi Graziano Leoni Angelo Marcello Tarantino | 1996 | Journal of Structural Engineering1996，122，4： | 1 |
| 19 | A Model for the 3D Kinematic Interaction Analysis of Pile Groups in Layered Soils 显示文摘 | Dezi F Carbonari S Leoni G | 2009 | Earthquake Engineering and Structural Dynamics2009，38，11： | 1 |
| 20 | Complications of laparoseopie eholeeystectomy a national survey Of 1292 hospitals and an analysis of 77604 cases 显示文摘 | Dezie DJ Millikan KW Eeonomous SG | 1993 | Sarg1993，165，： | 1 |
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