北呂宋島弧系列的地質研究對於了解台灣的地質歷史是一個很重要的材料，自然界中的岩礦可以記錄許多訊息，例如自然界中的磁性礦物可以保留當下古地磁的方向以及其強度，但因為岩石複雜的化學組成成分，在自然界中的風化與化學作用影響，許多訊息都變得更加複雜且難以運用。因此本研究藉由岩石磁學、岩象學分析、地球化學分析及實驗室模擬合成等方法，將複雜的問題抽絲剝繭合理解釋並進一步推論出結果。本研究以綠島公館鼻熔岩流為例，初步的岩石磁學分析發現同一個地點記錄到多種古地磁紀錄，有穩定正向、隨著熱退磁正向反向自我反轉與穩定反向三種古地磁記錄模式。為了探討多種古地磁紀錄造成的原因，由光薄片觀察其微觀礦物組織之異同，再運用地球化學分析了解不同古地磁紀錄的岩層是否因不同的化學成分組成所導致。從本研究中發現雖然所含的磁性礦物皆為貧鈦的磁赤鐵礦，但因為氧化程度的不同造成礦物磁特性的差異。亦即貧鈦磁赤鐵礦在加熱過程中會造成結構的改變導致岩石磁學的反轉。在絕對強度上，本研究發現微觀與巨觀的趨勢有著正相關的連結，也許在探討巨觀古地磁的絕對強度時，磁力顯微鏡可以是個不錯的工具提供不一樣的研究資訊，在古地磁或是地質領域上可以提供相關的協助及研究。而與合成礦物相互比較，發現在顆粒小於3000 nm時，磁區模式皆為單磁區，比巨觀磁性所推測的臨界半徑大，因此在自然界中能觀測到擬單磁區的情形，在實驗室合成顆粒亦能觀察到。

Rock magnetic properties including remanent magnetization、magnetic susceptibility and magnetic coercivity .All of them are controlled by magnetic mineral in the rock. Therefore, comprehend mineral magnetism is important section to interpret rock magnetic properties. In this study we focus on magnetic mineral in Gonguanbi andesite. First, we find out there are three result in nature remanent magnetization (NRM)(a) stable normal polarity in case GN163、GN165、GN171.(b)Self-reverse in 320℃、360℃ in case GN167.(c) stable reversal polarity in case GN168、GN169. Second, we identify mineral phases in Gonguanbi andesite by X-ray Diffractometer and X-ray photoelectron spectroscopy. Magnetic mineral in Gonguanbi is maghemite. Because XRD characteristic peak (3 1 1) at 35.5∘is more near XRD characteristic peak (311) 35.6∘of maghemite. We also confirm mineral phase by X-ray photoelectron spectroscopy (XPS). Fe3+and Fe2+ composition ratio in Gonguanbi is 95/5. Magnetite Fe3+and Fe2+ composition ratio is 67/33, Maghemite Fe3+and Fe2+ composition ratio is 100/0. So, we confirm magnetic mineral in Gonguanbi is maghemite. However, we observe MFM in Gonguanbi sample more than 95% magnetic mineral are multi-domain. It is different from Penghu.

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