理學院

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學院概況

理學院設有數學系、物理學系、化學系、生命科學系、地球科學系、資訊工程學系6個系(均含學士、碩士及博士課程),及科學教育研究所、環境教育研究所、光電科技研究所及海洋環境科技就所4個獨立研究所,另設有生物多樣性國際研究生博士學位學程。全學院專任教師約180人,陣容十分堅強,無論師資、學術長現、社會貢獻與影響力均居全國之首。

特色

理學院位在國立臺灣師範大學分部校區內,座落於臺北市公館,佔地約10公頃,是個小而美的校園,內含國際會議廳、圖書館、實驗室、天文臺等完善設施。

理學院創院已逾六十年,在此堅固基礎上,理學院不僅在基礎科學上有豐碩的表現,更在臺灣許多研究中獨占鰲頭,曾孕育出五位中研院院士。近年來,更致力於跨領域研究,並在應用科技上加強與業界合作,院內教師每年均取得多項專利,所開發之商品廣泛應用於醫、藥、化妝品、食品加工業、農業、環保、資訊、教育產業及日常生活中。

在科學教育研究上,臺灣師大理學院之排名更高居世界第一,此外更有獨步全臺的科學教育中心,該中心就中學科學課程、科學教與學等方面從事研究與推廣服務;是全國人力最充足,設備最完善,具有良好服務品質的中心。

在理學院紮實、多元的研究基礎下,學生可依其性向、興趣做出寬廣之選擇,無論對其未來進入學術研究領域、教育界或工業界工作,均是絕佳選擇。

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    Structural and metamorphic evolution of the Day Nui Con Voi massif, Northeast Vietnam
    (2015) 丁氏 惠; Hue-Thi Dinh
    The Day Nui Con Voi massif in North Vietnam is the southernmost part of the Red River Shear Zone in Southeast Asia. It is a narrow NW-SE trending high-grade metamorphic zone composed of amphibolite, migmatite, mylonite and gneiss. Structural analyses suggest that Day Nui Con Voi experienced at least 3 generations of ductile deformation. The oldest Dn-2 event formed NNW-SSE striking upright folds. The Sn-2 foliations parallel sillimanite and mymerkite indicated the Dn-2 event should occurred around amphibolite facies (>600 °C) metamorphic condition. The Dn-1 event is associated with subhorizontal folds with subhorizontal fold axial plane Sn-1 within the central region of the massif. The mineral assemblages of sillimanite + biotite + quartz + plagioclase + K-feldpar + muscovite suggest that the temperature of Dn-1 deformation is around 600 to 550°C. The Dn-1 structures are refolded by Dn, which formed a dome like structure with NW-SE striking Sn fold axial plane. Sillimanite boudinage necks filled by muscovite indicates that the Dn happened at lower temperature (<550oC). The youngest ductile deformation formed mylonite zone with left-lateral kinematic indicators on both limbs of the dome. Structural and petrological analyses suggest that left-lateral shearing happen synchronously with doming event (Dn deformation). Our new 40Ar/39Ar age data shows the cooling age of hornblende about 26 Ma, phlogopite from 23 to 24 Ma and K-feldspar from 21 to 23 Ma. Muscovite represents the age of both cooling and crystallization ages from 22 to 24 Ma. Basing on different age of different minerals relating to different closure temperatures, cooling history of the Day Nui Con Voi massif is reconstructed. Combining results of petrological analyses and cooling history, we constrains that left-lateral shearing event likely occurred during 26 ~ 22 Ma causing rapid cooling of the massif. From these conclusions, we propose that strike slip movement along Red River Shear Zone may not relate to opening of the South China Sea.