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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
51

Civic centre in Ma On Shan

許秀玲, Hui, Sau-ling, Emilie. January 1997 (has links)
published_or_final_version / Architecture / Master / Master of Architecture
52

The re-search of place and placelessness in Shan Ha Tsuen: a traditional village in Ping Shan

Yeung, Wai-fung, Jacky., 楊偉峰. January 2000 (has links)
published_or_final_version / Architecture / Master / Master of Architecture
53

Inter-modal coordination of Ma On Shan Rail with other public transport modes

Hue, Ka-yiu., 許家耀. January 2005 (has links)
published_or_final_version / abstract / Transport Policy and Planning / Master / Master of Arts in Transport Policy and Planning
54

Natural terrain landslide study in Lung Fu Shan area

Cheung, Wah-fung., 張華峰. January 2007 (has links)
published_or_final_version / abstract / Applied Geosciences / Master / Master of Science
55

Environmental awareness spiritual park at Lau Fau Shan

Pang, Shun-chin., 彭順千. January 2007 (has links)
published_or_final_version / abstract / Architecture / Master / Master of Landscape Architecture
56

閻錫山與抗戰

陳曉慧, CHEN, XIAO-HUI Unknown Date (has links)
抗日戰爭動員全國、悲壯慘烈,使得許多地方軍人捐棄成見,一致投入這民族共同禦 外的戰爭。其中最顯而得見的是山西的閻錫山,他在抗戰中的表現與頁獻,是應該為 歷史所肯定的。 抗戰時期閻錫山被任命為第二戰區司令長官,無論在山西或是對於全國局勢,均有重 大的影響,是一位舉足輕重的人物,非常值得研究。本論文擬以時間為經、事件為緯 ,藉著分析事件的過程及影響,以突顯人物的重要。全文共分為六章。第一章敘述閻 錫山崛起山西的經過,在辛亥革命、北洋政府、北伐、中原大戰各時期他所扮演的角 色,可說是抗戰以前背景的描述,有助於以下數章的發展。第二章申述自九一八事變 至七七抗戰爆發期間,閻氏面對日軍積極侵華的應付、準備,及其抗日的決心,另亦 述及其建設山西的成效。第三章以第二戰區為主,說明閻氏在山西如何領導軍民抗戰 ,在困厄的環境中,支持到抗戰最後,始終未讓日軍渡過黃河。 第四章探討閻錫山與中共的關係,說明中共利用犧盟會和決死隊叛變,打擊閻氏,並 得以迅速擴張其勢力於華北的經過。第五章則研究抗戰時期日本對閻錫山「合作」的 試探,閻氏如何運用策略以保生存等。最後綜合各章節所舉事件之分析,在結論中為 抗戰時期的閻錫山做一整體性的評論客觀地給予歷史上的地位。 本論文所引用的資料,以國史館典藏「閻故資政錫山遺存檔案」為主,其次是閻錫山 的年譜、回憶錄、傳記,戰時出版品及有關的論著、報紙、期刊等,希望有助於對抗 日戰爭史的探究及對於閻錫山有更深刻的了解。
57

孫中山與中國傳統文化之現代化

陳紹菁, CHEN, SHAO-JING Unknown Date (has links)
本論文的重點在討論近代中國文化巨大的轉變過程中,傳統文化是否有礙於中國的現 代化,中國要現代化是否必須將中國傳統文化放棄,以及孫中山先生如何在中國文化 的衰頹危機中,平衡了中國人理智與感情的衝突掙扎,以銜按中國的傳統與現代,為 中國傳統文化之現代人化而努力。 本論文共分為六章十七節,第一章:「緒論」,共分三小節,分別敘述研究的動機、 研究的方法以及研究的範圍。第二章:「近代西方文化的挑戰與中國的回應」,亦分 三節,分別敘述有關文化的定義、文化的變遷理論,以及西方文化東漸之後,對中國 文化所產生的衝擊,中國為因應此一新情勢,而展開了各種文化變革運動,依其時間 先後劃分為五大歷程討論。第二章:「現代化過程中傳統文化的危機」,共分三節, 敘述近百年來中國傳統文化遭受到的打擊與破壞,依時間先後,劃分為三個最具代表 性時期討論,其一是清末傳統文化面臨轉型初期的情形,其二為五四新文化的反傳統 運動,其三則是中共政權對中國文化的全面攻擊與破壞。第四章:「傳統與現代關係 之探討」,共分二節,第一節由學理上綜合。分析傳統與現代之間的關係是否必然對 立,第二節則分析孫中山先生思想中對傳統文化與現代化的態度。第五章:「孫中山 先生與中國傳統文化之現代化」,共分三節,分別從民族、民權以及民生三方面敘述 中山先生如何作為中國傳統與現代之橋樑,為中國傳統文化之轉換以適合現代潮流而 努力。第六章:「結論」亦分三節,其一比較近代中西文化之特質與差異之原因,其 二評估孫中山先生對中國文化的貢獻,最後並反省中國文化的現化意義。
58

孫中山先生與護法運動( 一九一七∼一九二三)

姚誠, YAO, CHENG Unknown Date (has links)
緒論 第一章 護法運動的源起 第一節 護法運動發生的歷史背景 第二節 中山先生號召護法之目的 第二章 軍政府大元帥時期 第一節 護法軍政府的成立 第二節 軍政府的困境 第三節 軍政府的改組 第三章 離粵赴滬時期 第一節 護法政府名存實亡 第二節 南北和會的召開及影響 第三節 中山先生與新文化運動 第四節 革命理論的奠基─建國方略 第章章 正式政府非常大總統時期 第一節 重振護法聲威─粵軍回粵 第二節 組織正式政府的經過 第三節 中山先生與聯省自治 第四節 中山先生廣州蒙難 第五章 護法運動的終結 第一節 中山先生重回廣州 第二節 中山先生放棄護法 第六章 護法運動失敗的原因和影響 第一節 護法運動挫敗的反省 第二節 挫敗後的奮起─國民革命的再出發 結論
59

荀子哲學的反思:以人觀為核心的探討 / Reflections on the philosophy of the Xunzi: focusing on human nature

王靈康, Wang, Ling Kang Unknown Date (has links)
本文嘗試重建荀子哲學的人觀,並以此為核心,反思荀子哲學的歷史定位、其道德規範之依歸、道德哲學之性質、道德理想在修養與教化上扮演的功能,以及反思荀子哲學中人與世界的關係。首先指出歷來對荀子人觀的詮釋局限於性惡論,如此的詮釋在文獻依據與理論需求上均有待補充。隨後嘗試說明其道德哲學除了追求正理平治的社會生活之外,更可能還包括人格之提昇;而此分別以「善」之兩重意義為代表。在道德修養中,「聖」所扮演的角色也有兩重;一方面是作為修養方向的最高理想,另一方面是以具體的歷史人物作為典範。最後,在天人關係上,本文提出人能夠認識的世界,是「天」在人之經驗中呈現的現象,人據以認識世界、利用資源所需的自然法則,也是累積長久的觀察之後以某種建構方式得到的。
60

Paleoglaciology of the Tian Shan and Altai Mountains, Central Asia

Blomdin, Robin January 2016 (has links)
The mountain-systems of Central Asia, act as barriers to atmospheric circulation patterns, which in turn impose striking climate gradients across the region. Glaciers are sensitive indicators of climate change and respond to changes in climate gradients over time by advancing during cold and wet periods and receding during warm and dry periods. The aim of this thesis is to investigate whether there are large-scale patterns in how past glaciers in the Tian Shan and the Altai Mountains of Central Asia responded to climate change. Multiple methods have been used, including: remote sensing, terrain analysis, field investigations, and cosmogenic nuclide (CN) dating. The glacial landform records indicate that the region experienced mainly alpine-style glaciations in the past. Large complexes of ice-marginal moraines in high elevation basins are evidence of outlet glaciers sourced from large valley glaciers, ice caps and ice-fields, and these moraine sequences, record the maximum extent of paleoglaciation. In the Ikh-Turgen Mountains, located in the continental, eastern Altai Mountains, deglaciation of these moraines occurred during marine oxygen isotope stage (MIS) 3 at ~45 ka. This is consistent with a colder and wetter climate during this time, inferred from ice core and lake level proxies. Another deglacial phase occurred during MIS 2 at ~23 ka, synchronous with the global Last Glacial Maximum. In the Russian Altai Mountains, lobate moraines in the Chuya Basin indicate deglaciation at ~19 ka, by a highly dynamic paleoglacier in the Chagan-Uzun catchment, which experienced surge-like behaviour. Furthermore, across the Tian Shan, an evaluation of new and existing CN glacial chronologies (25 dated moraines) indicates that only one regional glacial stage, between 15 and 28 ka (MIS 2), can be defined and spatially correlated across the region. These paleoglaciers were mainly restricted to valleys as a result of arid conditions during this time and variation in their extents is interpreted to reflect topographic modulation on regional climate. The ages of the oldest evidence for robust local glacial stages in the Tian Shan are not yet well constrained, however, moraines in the central Kyrgyz Tian Shan and the eastern Chinese Tian Shan have apparent minimum ages overlapping with MIS 5 and MIS 3 (with missing MIS 4 and 6 stages). However, different geological processes, such as inheritance and post-depositional shielding (e.g. deposition by surging glaciers or hummocky terrain deposition), have influenced the dating resolution, making several moraine ages inappropriate for regional comparison. Finally, to quantify regional patterns of paleoglaciation, the hypsometry (area-elevation distribution) of glacial landforms is used to estimate average paleo equilibrium line altitudes for the region. This analysis shows that while present-day ELAs mirror strong climate gradients, paleoglaciation patterns were characterised by more gentle ELA gradients. The paleo-ELA depressions across Central Asia were most prominent in the continental southern and eastern regions (500–700 m). Finally, the results from this thesis, show that Central Asia was repeatedly glaciated in the past, but underscore the importance of considering 1) catchment characteristics and styles of glaciation and 2) other non-climatic factors controlling glacier dynamics when interpreting CN chronologies to make paleoclimate inference. / <p>At the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 2: Manuscript. Paper 4: Accepted. Paper 5: Manuscript.</p> / Central Asia Paleoglaciology Project (CAPP)

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