黃金及住在一起的礦物左鄰右舍
黃金及住在一起的礦物左鄰右舍
2022/07/27
2022/09/26
金瓜石-九份金礦山常見的脈石礦物<br><br><i>本展為《</i><a target="_blank" rel="nofollow" href="https://openmuseum.tw/muse/exhibition/f15d166bcb680e3847ce38761d4ccf11"><i>黃金山城地質趣</i></a><i>》子章節,歡迎前往該展了解更多相關知識。</i>
展覽頁面呈現形式
橫式
策展者
國立臺灣博物館
展覽封面
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展覽資料
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"desc": "金瓜石-九份金礦山常見的脈石礦物<br><br><i>本展為《</i><a target=\"_blank\" rel=\"nofollow\" href=\"https://openmuseum.tw/muse/exhibition/f15d166bcb680e3847ce38761d4ccf11\"><i>黃金山城地質趣</i></a><i>》子章節,歡迎前往該展了解更多相關知識。</i>",
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"desc": "<div>金瓜石-九份金礦山常見的脈石礦物有石英、重晶石、明礬石、白鐵礦、方解石、菱錳礦、閃鋅礦、方鉛礦、辰砂、自然汞、自然硫、臭蔥石、石膏、膽礬等。除了礦體中的礦物之外,金瓜石-九份地區常見的安山岩中,也有些漂亮且有趣的礦物值得介紹,例如黑雲母、角閃石、磁鐵礦及鋯石,也將在後文中介紹。是一個著名的金銅礦區,也出產了許多全臺特有的礦物,接下來我們將為您介紹一些這個地區常見的礦物。</div><div><br></div><div>下次當您在野外發現這些美麗的礦物時,您除了可說出它們的名字外,也將對它們在大地舞臺演化過程中或對人類科技與文明的貢獻扮演的角色讚嘆不已。</div>",
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"desc": "早期的採金者或銀樓業者便常利用黃金顏色來判定其純度,他們使用一種磨平的黑色細緻的硬頁岩結核,俗稱「試金石」者,將金在它上面輕輕劃線,如果是純金,劃出來的線會有點偏紅,而18K金的線,看起來便有點白了。這個方法雖然不是十分準確,但卻也是非常方便實用的一個方法。",
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"desc": "黃金具有非常高的延展性,通常可由其特殊的金黃色及延展性可切性加以鑑別。它很容易與黃銅礦及黃鐵礦(俗稱「愚人金」)混淆,但是黃鐵礦較硬,顏色較白,條痕是黑色的,而黃銅礦雖然硬度也不大,但是較脆,從這些特性都可以加以區別。另外,某些絹雲母或受風化的黑雲母碎片也常常容易被誤以為是黃金,但是雲母類礦物用指甲尖或刀片很容易壓破,並且這些礦物很輕,在水中淘洗也可以馬上加以區分。",
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"desc": "硫砷銅礦的晶體常聚集叢生成晶簇,生長在礦脈或岩洞中,在現今本山、樹梅、第一長仁、第三長仁及牛伏等許多礦體的地表露頭均仍可尋得它們的蹤跡。",
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"desc": "<span>在金瓜石-九份地區,地表附近的黃鐵礦結晶較小,一般只有0.05~0.2公分大,以正立方體、正八面體較常見。而在地底深處,黃鐵礦的晶體較大,且以正八面體為主,在本山的八坑(大約海平面下約132公尺)曾發現邊長達10公分的黃鐵礦正八面體晶體。<span><br>\n<br>\n</span>除了晶體大小及晶型會隨深度有所變化以外,黃鐵礦內部微量元素的含量也會隨深度而有所變化,根據研究顯示,在金瓜石地底深部黃鐵礦含有較多的銅、砷、鈷及鎳,而淺部的黃鐵礦則一般含較多的銀、鉛及鋅。</span>",
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"desc": "黃鐵礦的主要成分為硫化鐵,早期常被用來作為製造硫酸的原料,另外,金礦地區的黃鐵礦經常含有黃金,例如根據筆者的研究指出,小金瓜附近的黃鐵礦含金可達100ppm,此種含金的黃鐵礦也是提煉黃金的重要材料,但黃鐵礦要提煉黃金前必須先經過鍛燒。早期金瓜石的黃鐵礦便曾先送往臺灣肥料公司作為製造硫酸鹽肥料的原料,然後礦渣再運回金瓜石煉金,最後剩餘的鐵渣還可也當製造水泥的副原料呢,可以說是一魚三吃!",
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"desc": "比較值得一提的是金瓜石的安山岩內具有一種較特殊的「高溫石英」,它是一般石英的同質異構礦物,具有與一般石英相同的化學成分,但結晶結構不同。高溫石英的外形以十二面雙錐體為主,但有時稜角會被磨去而略約成圓形,大小約0.2~0.5公分,顏色透明至白色,散布在本山等安山岩體中。石英由於性質穩定,在安山岩受到熱水礦化作用時不易發生變化,因此不管是新鮮的安山岩或者是受過矽化作用、黏土化作用或綠泥石化作用的安山岩內,均可發現「高溫石英」的蹤跡。如果想要蒐集高溫石英晶體的話,可以在較軟的黏土化安山岩內挑取。",
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"desc": "<span>另外金瓜石地區許多矽化作用的岩石,主要成分也都是石英物質,但多是微晶質(結晶顆粒非常微小)的二氧化矽礦物,或者稱為石髓。這種微晶質的石髓通常是白至灰色,但有時會因含雜質而呈黃色或黑色。這些不同顏色的石髓相混,常顯現出漂亮的圖案,也頗具可觀性。<span><br>\n<br>\n</span>少數結晶漂亮的石英(或稱水晶),只有在此地區局部岩石孔洞或裂隙中出現,但其晶體通常不大。石英除了是重要的寶石和飾品,也是非常重要的工業材料,因為它具有壓電和焦電性質,可以應用於壓力計、震盪器、共振器、穩波器等。而因其偏光性質,亦可用於製作偏光鏡。另外,石英可以使紫外光穿透,所以也可以用於一些特殊的稜鏡、透鏡和光學儀器等。石英被大量用於製造玻璃、顏料、研磨材料、陶瓷、耐火材料,及一些精密儀器等。石英製成的碳化矽為非常堅硬的研磨材料。</span>",
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"desc": "<span>金瓜石除了有結晶的明礬石以外,當然也有許多土狀(粉狀)的明礬石,它的顏色是白色的,外形和一般白色黏土礦物不易區別,通常須要在實驗室配合儀器才得以鑑定。<span><br>\n<br>\n</span>另外由於明礬石含有多量之鉀,是適宜做鉀-氬或氬-氬定年之材料,可以用來測定礦體的生成年代。在國立臺灣大學地質科學研究所便設置有質譜儀,可以進行氬-氬同位素定年法分析。</span>",
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"desc": "金瓜石地區角礫岩礦筒內的明礬石曾經筆者用上述的方法定年,其結果顯示角礫岩礦體的生成年代約為95萬年前,誤差範圍為一萬年(0.01百萬年),這個誤差範圍比起目前其他定年方法的十萬年(0.1百萬年)誤差精確許多,可以作為研究金瓜石地區礦床生成歷史更佳的工具。",
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"desc": "<span>由於白鐵礦主要是在強酸性溶液及低溫環境下生成的,而黃鐵礦則可在較廣泛的溫度下,從酸或鹼性溶液中生成,生長的條件較白鐵礦寬廣,所以白鐵礦的數量及分布均遠不如黃鐵礦。白鐵礦也比黃鐵礦容易風化變化成褐鐵礦及四水白鐵礬等礦物。<span><br>\n<br>\n</span>白鐵礦在九份及武丹山一帶的金脈中較多,在金瓜石金水公路的迴頭彎及樹梅南邊武丹坑均曾發現白鐵礦。它們的顏色呈灰色,一般具有腎狀的外形以及放射性的構造。</span>",
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"title": "方解石 (Calcite)",
"desc": "<span>方解石的英文名稱Calcite一字來自拉丁語的calx,指燒石灰(Burntlime)。方解石也是非常普遍的礦物,例如大家所熟悉的大理岩,主要便是由方解石礦物構成的。方解石具有非常強的雙折射性,透過其透明晶體觀看緊貼晶體後方的文字或圖案,會變成雙重影像,非常有趣。但是漂亮的結晶並不常見。<span><br>\n<br>\n</span>金瓜石地區的方解石一般都是白色並且少有漂亮的結晶,它們多產在九份、武丹山一帶的礦體。在本山及角礫岩礦筒地區,則要在離礦體較遠的地方才可以發現。方解石通常呈薄層生長在礦脈中,或充填於岩石裂隙中。</span>",
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"desc": "<span>白色且不具晶形的方解石,外表很像石英,在野外可以用硬度或稀鹽酸加以區別。方解石的硬度只有3,用小刀片(硬度約為5.5)便可很容易刮下粉末,而石英的硬度高達7,無法用小刀刮傷。<span><br>\n<br>\n</span>另外方解石碰到稀鹽酸會產生很多氣泡,而將稀鹽酸滴在石英上則不會有任何反應。<span><br>\n<br>\n</span>方解石對人類的貢獻也很大,透明的晶體可製成偏光鏡。組成一般石灰岩或大理岩則為重要的工業原料,如水泥、助熔、肥料、化工等用途。而結晶好且緻密的大理岩及石灰岩也可當建材、雕塑或飾品使用。</span><br>",
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"desc": "閃鋅礦只有在九份及武丹山一帶的金礦脈中發現,一般呈暗黃褐色或暗紅色粒狀產出,破裂面的顏色較淡。",
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"title": "請輸入頁面標題",
"desc": "<span>它和呂宋銅礦是屬於「異質同形」礦物(Isostructural),所謂「異質同形」是指兩個礦物的化學成分不同,但卻具有相似的結晶構造。法馬丁礦的化學成分是Cu₃SbS₄而呂宋銅礦則為Cu₃AsS₄,兩者的差別在於一個含銻,而另一個含砷,但兩者卻具有相似的結晶構造,同屬於正方晶系。<span><br>\n<br>\n</span>法馬丁礦在世界上產出的地點很少,且產量亦不多,通常無法單獨成為煉銅的主要礦物。但因為其稀有性,法馬丁礦卻常成為各博物館蒐集的對象。根據研究金瓜石金銅礦權威的臺大地質研究所譚立平教授表示,金瓜石所發現的法馬丁礦結晶,可能是世界上最漂亮的。</span>",
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"desc": "金瓜石產出法馬丁礦的地點多位於坑內,在地表尚未有發現的報導,因此除非金瓜石礦區重新開採,我們是很難在野外一窺漂亮的法馬丁礦。",
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"desc": "方鉛礦是金屬鉛的主要來源,另外由於方鉛礦常含有銀,因此也常成為重要的銀來源。在基隆河中淘洗砂金時,時常可以發現銀白色發亮的方鉛礦,由於它的比重很大(7.4~7.6),因此不容易被沖走。您若有放大鏡,不妨仔細觀察一下,看能不能觀察到它漂亮的正立方體的晶面。",
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"title": "辰砂 (Cinnabar)",
"desc": "<div>辰砂也叫朱砂,有時又被稱為丹砂,化學成分HgS,是主要的煉汞原料。其英文Cinnabar一詞源自波斯文「zinjifrah」(失落),其命名緣由可能和神話有關。</div><div><br></div><div>它經常呈現出非常鮮豔漂亮的紅色,有名的印材「朱砂凍」,便是因含有辰砂而顯得驕豔動人。</div>",
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"desc": "金瓜石的辰砂常形成葡萄狀集合體或小粒狀,顆粒通常在0.3公分以下,以角礫岩礦筒地區產出較多。由於它的比重很大,在淘洗砂金時很容易發現它。",
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"title": "請輸入頁面標題",
"desc": "在金瓜石南方不遠的雙溪區平林村是臺灣唯一曾開採水銀礦的地點,當地的水銀礦石主要便是辰砂。",
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"title": "自然汞 (Native Mercury)",
"desc": "自然汞(或稱水銀)其英文名稱Mercury源自羅馬神話當中神的名字Mercurius。水銀是一種引人爭議的「礦物」,因為根據礦物學的定義,礦物必須為固體,所以有人認為它不是礦物,但也有部分礦物學家將它列為礦物之列,在此我們不去討論它是不是一種礦物。",
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"title": "自然汞比重很大,甚至可以將鐵浮起",
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"desc": "水銀在常溫下是液體,比重很大,由於它的表面張力極大,因此常呈圓珠狀。在金瓜石竹礦體附近的地表土壤中,曾發現許多的水銀。根據許多資深礦工陳述,以前在竹礦體附近山坡挖掘土壤,有時便可看見水銀流出。另外,在第一長仁礦體內部,也有自然汞的發現。",
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"desc": "<div>在金瓜石南方雙溪區的平林村,也曾發現河川沉積物中許多自然汞,筆者等在當地淘洗砂金時,便曾淘到自然汞。由於自然汞會將金溶入,變成汞膏(almagam),因此如果您在淘金時,在淘金盤內同時淘到水銀及砂金時,最好儘速分離兩者,否則再淘下去,砂金便可能會被水銀溶掉了。</div><div><br></div><div>水銀除了常作為汞膏以回收黃金或白銀,工業上還可用於製造炸藥、電子工業整流器、醫療用品等。</div>",
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"desc": "<div>普通角閃石和黑雲母同樣在熱水換質作用中容易發生變化。在矽化的安山岩內,普通角閃石完全被溶走,只剩下長柱體的外型;在黏土化安山岩中,它已轉變成灰色黏土礦物;而在綠泥石化安山岩中,它的外表看似不變,但實際上也多多少少被綠泥石所換質了。</div><div><br></div><div>普通角閃石並無工業用途,但由於晶形漂亮特殊,常成為玩石家及地質學家所喜愛蒐集的礦物。</div><div><br></div>",
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"desc": "<div>由於鋯石中常含有少量的放射性元素-鈾238,這些放射性元素會產生核分裂,而它們分裂後的兩個新原子核會以極高的速度分離,並在鋯石內部它們所經過的路徑產生形成放射性傷害,地質學家稱這種傷害痕跡為「核飛跡」。核飛跡的數量會隨著年代的變老,而逐漸累積增加,因此,只要能算出鋯石中單位面積內核飛跡的數目,並且經由中子照射,推算出鋯石原始的鈾含量,便可以知道鋯石或者火成岩的生成年代了。</div><div><br></div><div>金瓜石-九份地區各個安山岩的年代,經由鋯石核飛跡計算的結果,大約是在140萬年前到90萬年前,聽起來好老,但是在地質年代而言,它們都還算非常年輕呢。不過由於核飛跡非常小,必須先以化學試劑加以腐蝕,並且在1000倍的顯微鏡下才可以觀察的到,因此在野外是看不到的。</div>",
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