224,819 research outputs found
Zhou li zheng yi
No full text"Zhou li" yuan ming "Zhou guan". shi ni ding Zhou dai guan zhi de zhu zuo, bei feng wei ru jia jing dian zhi yi, nei rong fen tian guan, di guan, chun guan, xia guan, qiu guan, dong guan liu da bu fen, qi zhong dong guan yu han chu wang yi, bu zhi yi "Kao gong ji". "Zhou li zheng yi" shi Qing dai zhu ming xue zhe Sun Yirang zai Han dai Zheng Xuan zhu, Tang dai Jia Gongyan shu de ji chu shang dui "Zhou li" ia yi kao zheng shu jie zhi zuo, hu zhong bo cai zhong shuo,zi liao fan fu, kao zheng jing xiang, dui yan du zhou li"yi shu, ji you can kao jia zhi, Ci ci jing guo Wang Shaohua xian sheng dian xiao zheng li, zhi liang geng shang ceng lo
Bu nong yu dan qun fang yan fen lei ci hui shou ce /
No full textBen shu gen ju xian dai bu nong yu dan qun ma yuan fang yan de kou yin diao cha, Bian ji er cheng, Jiang chang yong ji ben ci hui jin xing bian ji zheng li, Gong fen wei"shu zi", "ren cheng dai ci", "yi wen ci", "fang xiang yu di ming"deng ji ge xiang mu.Ben shu gen ju xian dai bu nong yu dan qun ma yuan fang yan de kou yin diao cha, Bian ji er cheng, Jiang chang yong ji ben ci hui jin xing bian ji zheng li, Gong fen wei"shu zi", "ren cheng dai ci", "yi wen ci", "fang xiang yu di ming"deng ji ge xiang mu.Taiwan resource centre for Chinese studie
Xiang ju
No full text陳碨, 顏招治口述 ; 顏梓和, 王遊治, 黃海瑞整理.根據陳碨, 顏招治口述, 薌劇編導會議集體討論, 顏梓和等整理而成.Chen Wei, Yan Zhaozhi kou shu ; Yan Zihe, Wang Youzhi, Huang Hairui zheng li.Gen ju Chen Wei, Yan Zhaozhi kou shu, Xiang ju bian dao hui yi ji ti tao lun, Yan Zihe deng zheng li er cheng
Shi ren jue li xiang jie
No full text[v.1-2]. 目錄 -- [v.2-8]. 五言古詩 : 二十四卷 -- [v.9-11]. 七言古詩 : 十三卷 -- [v.12]. 五言絶句 : 八卷 -- [v.13-14]. 七言絶句 : 十卷 -- [v.15-18]. 五言律詩 : 十五卷 -- [v.19-20]. 五言排律 : 十一卷 -- [v.21-22]. 七言排律 : 九卷 -- [v.23-26]. 唐詩拾遺 : 十卷.[v.1-2]. Mu lu -- [v.2-8]. Wu yan gu shi : er shi si juan -- [v.9-11]. Qi yan gu shi : shi san juan -- [v.12]. Wu yan jue ju : ba juan -- [v.13-14]. Qi yan jue ju : shi juan -- [v.15-18]. Wu yan lü shi : shi wu juan -- [v.19-20]. Wu yan pai lü : shi yi juan -- [v.21-22]. Qi yan pai lü : jiu juan -- [v.23-26]. Tang shi shi yi : shi juan.高棅編.綫裝, 4函.框21.9x15.5公分, 10行20字, 小字雙行同. 白口, 左右雙邊, 單黑魚尾. 版心中鐫"唐詩"及卷次.有洪武癸酉高棅序及洪武乙亥林慈序.With: 引用諸書 ; 歷代名公叙論 ; 詩人爵里詳節.Xian zhuang, 4 han.Kuang 21.9 x 15.5 gong fen, 10 hang 20 zi, xiao zi shuang hang tong. Bai kou, zuo you shuang bian, dan hei yu wei. Ban xin zhong juan "Tang shi" ji juan ci.You Hongwu gui you Gao Bing xu ji Hongwu yi hai Lin Ci xu.Gao Bing bian.With: Yin yong zhu shu ; Li dai ming gong xu lun ; Shi ren jue li xiang jie
Ma ke si jing dian zheng zhi jia zhi si xiang ji lu
No full textBen shu bi zhe zai zuo bo shi hou ke ti bao gao,Xiang mu yan jiu guo cheng zhong,Tong guo dui ma ke si jing dian wen xian de yan du,Jie he shi dai te zheng he xu yao,Dui qi zhong yun han de zheng zhi jia zhi si xiang ru fu qiang,Min zhu,Wen ming,He xie,Zi you,Ping deng,Gong zheng,Fa zhi,Ai guo,Jing ye,Cheng xin,You shan deng deng zuo le jiao wei xi tong de shu li,Zhai bian,Ji jie cheng shu,Zai xian ma ke si jing dian zhu zuo de li lun sheng ming li he xian shi gan zhao l
Book review “Analytics in smart tourism design”; Zheng Xiang, Daniel R. Fesenmaier
No full textBook review “Analytics in smart tourism design”; Zheng Xiang, Daniel R. Fesenmaie
A palaeogeographic context for Neoproterozoic glaciation
Full text linkPaul F. Hoffman and Zheng-Xiang L
Precambrian evolution and cratonization of the Tarim Block, NW China: petrology, geochemistry, Nd-isotopes and U-Pb zircon geochronology from Archaean gabbro-TTG-potassic granite suite and Paleoproterozoic metamorphic belt
No full textAbstract not availableChuan-Lin Zhang, Huai-Kun Li, M. Santosh, Zheng-Xiang Li, Hai-Bo Zou, Hongyan Wang, Haimin Y
Magmatic switch-on and switch-off along the South China continental margin since the Permian: Transition from an Andean-type to a Western Pacific-type plate boundary
No full textDetrital zircon provenance data for the Tananao schist in eastern Taiwan is consistent with its protolith being deposited on the South China continental margin at around, or soon after, 150 Ma, rather than being of an exotic origin and much older as previously suggested. The absence of ca. 200 Ma zircons agrees with the presence of a magmatic gap in the region after the orogenic and magmatic front migrated to central South China, due to a flat-slab subduction. The characteristic lack of input from interior South China (i.e., the lack of 1100–750 Ma and 470–420 Ma populations), and the immature nature of some of the schist units, suggest that they were sourced from the nearby coastal regions. On the other hand, they exhibit a dominant 190–150 Ma magmatic zircon population, suggesting the presence of abundant magmatic rocks of that age along the coastal regions. This, along with our newly discovered ca. 180 Ma I-type granites from eastern Zhejiang and other ca. 190–180 Ma magmatic rocks recently reported from the coastal regions, led us to propose that a new continental arc was initiated after ca. 190 Ma along the coastal region after a magmatic gap due to flat-slab subduction. This newly initiated arc likely persisted until ca. 90 Ma, and is represented by the I-type granitic rocks in eastern Taiwan. Slab roll-back likely caused the arc system to retreat towards the Pacific Ocean after 90 Ma, and ca. 60–17 Ma bimodal magmatism adjacent to the South China Sea signifies continental margin extension in the lead-up to, and during, the opening of the South China Sea. We thus argue that the continental margin of East Asia was transformed from an Andean-type plate margin at 280–90 Ma, to the present-day Western Pacific-type plate margin soon after 90 Ma
Replication Package for "Surges and Instability: The Maturity Shortening Channel"
No full textReplication folder for the paper entitled "Surges and Instability: The Maturity Shortening Channel" by Xiang Li and Dan S
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