本文選題：寶玉石礦床 + 成玉作用　； 參考：《地學(xué)前緣》2017年06期

【摘要】：寶石礦床學(xué)是礦床學(xué)與寶石學(xué)之間的交叉學(xué)科,是聯(lián)結(jié)寶石學(xué)與地質(zhì)學(xué)的重要紐帶。寶玉石是礦物巖石中的精美部分,是地球物質(zhì)中的組成部分,是探索地球組成、特征與演化的重要研究對(duì)象。隨著人們對(duì)寶玉石外觀特征、特性與效應(yīng)等成因認(rèn)識(shí)的深化和新的寶玉石種類被發(fā)現(xiàn)并應(yīng)用,寶玉石礦床學(xué)正在成長(zhǎng)為集地質(zhì)學(xué)與寶石學(xué)為一體的、內(nèi)容豐富的學(xué)科。在文中回顧了寶石礦床學(xué)的歷史與發(fā)展,總結(jié)了寶玉石資源的分布特點(diǎn),提出了寶玉石成礦作用并做了簡(jiǎn)要論述,給出了寶玉石礦床的特點(diǎn)及寶玉石礦床學(xué)的研究特征。認(rèn)為,寶石礦物或巖石的成礦作用是研究寶玉石礦床的基礎(chǔ),然而,要形成首飾級(jí)的寶玉石,還需要研究成寶、成玉作用。寶玉石中的很多特性與效應(yīng),如變彩、變色、變石、月光等效應(yīng)的成因機(jī)理及特殊結(jié)構(gòu)的研究還有待完善,而關(guān)于其在自然條件下形成機(jī)理等問題,很多是空白�？偟膩碚f,寶玉石礦床學(xué)研究?jī)?nèi)容還不完全、不夠系統(tǒng),很多寶石礦種的成因還停留在推測(cè)階段。預(yù)計(jì)在很長(zhǎng)時(shí)間內(nèi),寶玉石礦床學(xué)研究重點(diǎn)依然是單個(gè)礦床(已開采和新發(fā)現(xiàn)的)的資料收集與整理,不同產(chǎn)地同種礦物的寶玉石礦的類比與綜合分析。
[Abstract]:Gemstone ore deposit is an interdiscipline between ore deposit and gemology, which is an important link between gemology and geology. Baoyu stone is a fine part of mineral rocks and a part of earth material. It is an important research object in exploring the composition, characteristics and evolution of the earth. With the deepening of people's understanding of the appearance characteristics, characteristics and effects of Baoyu stone and the discovery and application of new types of Baojadeite, Baoyu ore deposit science is growing into a rich subject which integrates geology and gemology. In this paper, the history and development of gemstone ore deposit are reviewed, the distribution characteristics of Baoyu mineral resources are summarized, the metallogenic process of Baoyu stone is put forward, and the characteristics of Baoyu ore deposit and the research characteristics of Baoyu mineral deposit are given. It is considered that the mineralization of gem minerals or rocks is the basis of the study of Baoyu ore deposits. However, to form jewelry grade Baojite, it is necessary to study the role of treasure formation and jade formation. Many characteristics and effects in Baoyu stone, such as color change, stone change, moonlight effect and so on, need to be improved. However, many questions about the formation mechanism of Baoyu stone under natural conditions are blank. In general, the study of Baoyu ore deposit is not complete and systematic, and the genesis of many gem minerals is still in the stage of speculation. It is expected that for a long time, the emphasis of the study of Baoyu ore deposits will be the collection and collation of data of single ore deposits (mined and newly discovered), and the analogy and comprehensive analysis of the same minerals from different habitats.
【作者單位】： 中國(guó)地質(zhì)大學(xué)(北京)珠寶學(xué)院;中國(guó)地質(zhì)科學(xué)院地質(zhì)研究所;
【基金】：國(guó)家自然科學(xué)基金項(xiàng)目(41373055)
【分類號(hào)】：P619.281
，

本文編號(hào)：1927390