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| 1 | Zircon U-Pb SHRIMP ages of the Taiping (calc-alkaline)-Huangshan (alkaline) composite intrusion:Constraints on Mesozoic lithospheric thinning of the southeastern Yangtze Craton,China显示文摘The Taiping-Huangshan composite intrusion is a unique complex with characteristics changing from calc-alkaline (Taiping intrusion) to alkaline (Huangshan intrusion). Huangshan intrusion samples show a spectacular tetrad effect in their REE distribution patterns as well as non-CHARAC (charge-and radius-controlled) trace element behavior, indicating a highly evolved late-stage magma component. This composite intrusion provides a rare opportunity to investigate the variance of tectonic setting and lithospheric thinning of the southeastern Yangtze Craton in late Mesozoic era. Zircon SHRIMP U-Pb analyses yield an emplacement age of 140.6±1.2 Ma for the Taiping intrusion, and ages of 127.7±1.3, 125.7±1.4, 125.1±1.5, and 125.2±5.5 Ma for four samples from the Huangshan intrusion respectively. The ages for four different phases of the Huangshan intrusion agree within their small analytical errors, indicating that the emplacement was in a short time. The Taiping and Huangshan intrusions are intimately associated, but there is about 15 Ma interval between their intrusion, and the magma characters change from calc-alkaline to alkaline without transition. This probably corresponds to lithospheric thinning of the southeastern Yangtze Craton. This event possibly happened from about 141 Ma (the emplacement age of the Taiping intrusion), to 128 Ma (start of emplacement of the Huangshan intrusion). The thinning mechanism is dominantly delamination. | XUE HuaiMin WANG YingGeng MA Fang WANG Cheng WAN DeEn ZUO YanLong | 2009 | Science China Earth Sciences2009，52，11： | 28 |
| 2 | Microstructure and ^(29)Si NMR spectrum of Taiping orthoclase显示文摘Based on the study of 29Si,27Al NMR spectra for some orthoclases determined byX-ray powder diffraction method,Zhou et al.found that there are three maxima for the29Si NMR spectra of these orthoclases.In order to explain the three maxima the authorsexamined the 29Si NMR spectrum and microstructure of Taiping orthoclase occurring ingranitic dyke. | 薛纪越 周玲棣 郭九皋 李丽云 李齐 | 1996 | Chinese Science Bulletin1996，41，22： | 1 |
| 3 | 《太平广记》异僧小说的“三重”叙事显示文摘《太平广记》异僧小说整体上代表了晋唐时期僧传文学的叙事成就,有着宗教性、史传性和审美性三位一体的叙事特征。其神异叙事善于融通佛教哲思和启悟佛性体认;史传叙事注重烘托神异观念和突出宗教真实;审美叙事重视刻画僧人形象和描绘宗教神奇。 | 曾礼军 | 2014 | 辽东学院学报(社会科学版)2014，16，1： | 0 |
| 4 | Re-Defining the Late Qing Revolution:Its Continuity with the Taiping Rebellion,Radical Student Politics and Larger Global Context显示文摘Studies in recent decades conducted from the angle of provincial-level local self-government have done much to help relativize narratives of the 1911 Revolution in China that emphasize the importance of armed uprisings.However, these endeavors still have room to locate the revolution within a global context and to understand its implications as a revolution conducted through the conduits of culture and thought.More importantly,these existing studies are also insufficient in terms of viewing the Late Qing Revolution through a longer time span to see the Revolution as the new development and continuity of a much longer revolution that began with the Taiping Rebellion (1851-64).The Taiping Rebellion substantially weakened the rule of the Qing court.In other words,this author regards the Late Qing Revolution as a part of the long revolution starting from the outbreak of the Taiping Rebellion.Through this analysis,the author demonstrates how the Late Qing Revolution was comprised of three key components:armed uprisings,self-government movements,and finally,a revolution through words and culture including the student movements at home and in Tokyo.It argues that,to a certain degree,it is the Taiping Rebellion that made the Revolution successful in a relatively pacifistic way,and that,in particular,made possible the non-violent revolutions of self-government and the revolution through words and culture. | Lin Shaoyang | 2018 | Frontiers of History in China2018，13，4： | 0 |
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