本文選題：軟玉 + 次生礦物��； 參考：《石家莊經(jīng)濟(jì)學(xué)院》2015年碩士論文

【摘要】：軟玉作為一種中華民族文化傳承的媒介被流傳千年。軟玉開發(fā)利用悠久的歷史伴隨著整個(gè)華夏民族的發(fā)展歷程。軟玉根據(jù)產(chǎn)狀的不同被分為子料、山料、山流水,因經(jīng)過漫長的次生作用過程,子料(主要是其皮殼部位)的礦物成分及其結(jié)構(gòu)特征往往會(huì)發(fā)生一定程度的變化,給人感覺變得更細(xì)膩,且皮殼的顏色豐富,利用巧雕能使其更具藝術(shù)價(jià)值,所以帶皮子料往往更受到人們的喜愛。但是對(duì)于子料真假的鑒別還未能有一套理論用于指導(dǎo)實(shí)踐,對(duì)于軟玉的次生變化及次生礦物的研究尤其薄弱。本文針對(duì)這個(gè)問題選取了大量相關(guān)的軟玉樣品,主要對(duì)其次生礦物進(jìn)行系統(tǒng)的研究,對(duì)軟玉的研究工作進(jìn)行完善和補(bǔ)充。本文首先通過對(duì)大量軟玉樣品進(jìn)行手標(biāo)本的肉眼觀察及顯微觀察,分別對(duì)軟玉山料、子料及染色子料的外觀特點(diǎn)進(jìn)行總結(jié)和對(duì)比。然后選取特點(diǎn)鮮明的樣品做薄片進(jìn)行偏光鏡下的觀察,對(duì)次生礦物的結(jié)構(gòu)和存在形式做了研究,發(fā)現(xiàn)次生交代主要發(fā)生于表皮、裂隙及微裂隙附近,以及礦物顆粒結(jié)合不夠緊密的部分。裂隙、微裂隙為次生交代提供了通道。次生礦物集合體形態(tài)常表現(xiàn)為沿裂隙的脈狀、分散狀或保留原礦物的假象。利用多種現(xiàn)代測試技術(shù)如紅外光譜、X射線粉晶衍射、拉曼光譜和電子探針等,對(duì)發(fā)現(xiàn)的次生礦物進(jìn)行礦物成分的測試分析,發(fā)現(xiàn)軟玉石礓中被交代礦物為透輝石,交代礦物透閃石形成時(shí)間晚于軟玉主體(以透閃石為主,含有透輝石等)的形成,且質(zhì)地松散,也是一種次生礦物且存在較為普遍,山料子料中均可出現(xiàn);子料的皮殼和及其附近存在葉蛇紋石、綠泥石、滑石、方解石等次生礦物。葉蛇紋石、綠泥石、滑石等次生礦物組合出現(xiàn),是軟玉子料的標(biāo)型礦物組合。
[Abstract]:Nephrite as a medium for the cultural heritage of the Chinese nation has been circulated for thousands of years.The long history of development and utilization of nephrite is accompanied by the development of the whole Chinese nation.According to the occurrence of nephrite, it is divided into sub-material, mountain material and mountain flowing water. As a result of the long secondary process, the mineral composition and structural characteristics of the sub-material (mainly the part of its crust) often change to a certain extent.It makes people feel more delicate, and the color of the skin shell is rich, the use of artistry can make it more artistic value, so leather materials are often more popular.However, there is not a set of theory to guide the practice, especially for the secondary change of nephrite and the study of secondary minerals.In this paper, a large number of related samples of nephrite were selected, and the secondary minerals were studied systematically, and the research work of nephrite was improved and supplemented.In this paper, through the naked and microscopic observation of hand samples of a large number of nephrite samples, the appearance characteristics of nephrite material, sub-material and dyed sub-material were summarized and compared respectively.The structure and the existing form of secondary minerals are studied. It is found that the secondary metasomatism mainly occurs near the epidermis, cracks and microcracks, and the secondary metasomatism occurs mainly near the epidermis, fissures and microcracks, and the secondary metasomatism occurs mainly near the epidermis, cracks and microcracks.And mineral particles that are not tightly bound.Fissures, microcracks provide a channel for secondary metasomatism.The morphology of secondary mineral aggregates is often shown as veins along the fissure, dispersion or false retention of the original minerals.By using a variety of modern testing techniques such as infrared spectrum X-ray powder diffraction, Raman spectrum and electron probe, the mineral composition of the discovered secondary mineral was tested and analyzed. It was found that the metasomorphic mineral in the soft jade was diopside.The metasomatic mineral tremolite was formed later than the main body of nephrite (mainly tremolite, containing diopside and so on), and its texture is loose.There are secondary minerals such as serpentine, chlorite, talc, calcite and so on.The secondary mineral assemblages of serpentine, chlorite and talc are the standard mineral assemblage of nephrite.
【學(xué)位授予單位】：石家莊經(jīng)濟(jì)學(xué)院
【學(xué)位級(jí)別】：碩士
【學(xué)位授予年份】：2015
【分類號(hào)】：P619.281

【參考文獻(xiàn)】

中國期刊全文數(shù)據(jù)庫 前10條

1 劉晶,崔文元;中國三個(gè)產(chǎn)地的軟玉(透閃石玉)研究[J];寶石和寶石學(xué)雜志;2002年02期

2 廖宗廷,周征宇;軟玉的研究現(xiàn)狀、存在的問題及發(fā)展方向[J];寶石和寶石學(xué)雜志;2003年02期

3 廖任慶,朱勤文;中國各產(chǎn)地軟玉的化學(xué)成分分析[J];寶石和寶石學(xué)雜志;2005年01期

4 亓利劍;袁心強(qiáng);曹姝;;寶石的紅外反射光譜表征及其應(yīng)用[J];寶石和寶石學(xué)雜志;2005年04期

5 韓磊;洪漢烈;;中國三地軟玉的礦物組成和成礦地質(zhì)背景研究[J];寶石和寶石學(xué)雜志;2009年03期

6 李舉子;吳瑞華;凌瀟瀟;李青會(huì);;和田軟玉的化學(xué)成分和顯微結(jié)構(gòu)研究[J];寶石和寶石學(xué)雜志;2009年04期

7 潘小青;沈忠悅;張志亮;俞丹燕;;一種斜綠泥石質(zhì)仿田黃[J];寶石和寶石學(xué)雜志;2011年03期

8 劉長青;劉越陽;蔡新華;;拉曼光譜在玉石鑒定中的應(yīng)用[J];湖南文理學(xué)院學(xué)報(bào)(自然科學(xué)版);2011年01期

9 李幼琴,江紹英,范文偉;蛇紋石族礦物的紅外光譜特征及其研究[J];地質(zhì)科學(xué);1981年03期

10 趙虹霞;干福熹;;不同產(chǎn)地軟玉的拉曼光譜分析及在古玉器無損研究中的應(yīng)用[J];光散射學(xué)報(bào);2009年04期

中國重要會(huì)議論文全文數(shù)據(jù)庫 前1條

1 陸太進(jìn);鄧平;張勇;馮曉燕;陳華;柯捷;楊似三;;中國新疆和田玉子料表面特征微細(xì)結(jié)構(gòu)的發(fā)現(xiàn)和成因探討[A];2011中國珠寶首飾學(xué)術(shù)交流會(huì)論文集[C];2011年

中國博士學(xué)位論文全文數(shù)據(jù)庫 前1條

1 盧保奇;四川石棉軟玉貓眼和蛇紋石貓眼的寶石礦物學(xué)及其譜學(xué)研究[D];上海大學(xué);2005年

中國碩士學(xué)位論文全文數(shù)據(jù)庫 前4條

1 張娜;軟玉自然沁色和人工作沁的對(duì)比研究[D];中國地質(zhì)大學(xué)（北京）;2007年

2 史淼;新疆和田碧玉的礦物學(xué)特征及成因初探[D];中國地質(zhì)大學(xué)(北京);2012年

3 秦瑤;青海墨色軟玉的寶石學(xué)特征及礦物組成研究[D];中國地質(zhì)大學(xué)（北京）;2013年

4 吳曉;翡翠的次生變化及寶石學(xué)意義[D];石家莊經(jīng)濟(jì)學(xué)院;2011年

，

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