[1] |
冯晓燕, 张蓓莉.青海软玉的成分及结构特征[J].宝石和宝石学杂志, 2004, 6(4):7-9. doi: 10.3969/j.issn.1008-214X.2004.04.002
CrossRef Google Scholar
Feng X Y, Zhang B L.Study on compositions and texture characteristics of nephrite from Qinghai Province[J]. Journal of Gems and Gemmology, 2004, 6(4):7-9. doi: 10.3969/j.issn.1008-214X.2004.04.002
CrossRef Google Scholar
|
[2] |
李冉, 廖宗廷, 李玉加, 等.青海软玉中硅灰石的确定及其意义[J].宝石和宝石学杂志, 2004, 6(1):17-19. doi: 10.3969/j.issn.1008-214X.2004.01.005
CrossRef Google Scholar
Li R, Liao Z T, Li Y J, et al. Wollastonite in Qinghai nephrite jade and its significance[J]. Journal of Gems and Gemmology, 2004, 6(1):17-19. doi: 10.3969/j.issn.1008-214X.2004.01.005
CrossRef Google Scholar
|
[3] |
汤红云, 钱伟吉, 陆晓颖, 等.青海软玉产出的地质特征及物质成分特征[J].宝石和宝石学杂志, 2012, 14(1):24-31. doi: 10.3969/j.issn.1008-214X.2012.01.006
CrossRef Google Scholar
Tang H Y, Qian W J, Lu X Y, et al.Geological and composition feature of nephrite from Qinghai Province[J]. Journal of Gems and Gemmology, 2012, 14(1):24-31. doi: 10.3969/j.issn.1008-214X.2012.01.006
CrossRef Google Scholar
|
[4] |
周征宇, 廖宗廷, 陈盈, 等.青海软玉的岩石矿物学特征[J].岩矿测试, 2008, 27(1):17-20. doi: 10.3969/j.issn.0254-5357.2008.01.005
CrossRef Google Scholar
Zhou Z Y, Liao Z T, Chen Y, et al.Petrological and mineralogical characteristics of Qinghai nephrite[J]. Rock and Mineral Analysis, 2008, 27(1):17-20. doi: 10.3969/j.issn.0254-5357.2008.01.005
CrossRef Google Scholar
|
[5] |
李云峰, 高敏, 王悠然.青海软玉的宝玉石学特征及成因分析[J].现代矿业, 2014, 28(3):54-58. doi: 10.3969/j.issn.1674-6082.2014.03.016
CrossRef Google Scholar
Li Y F, Gao M, Wang Y R.The characteristics and genetic analysis of nephrite in Qinghai Province[J]. Modern Mining, 2014, 28(3):54-58. doi: 10.3969/j.issn.1674-6082.2014.03.016
CrossRef Google Scholar
|
[6] |
Yu H Y, Wang R C, Guo J C, et al.Study of the minerogenetic mechanism and origin of Qinghai nephrite from Golmud, Qinghai, Northwest China[J]. Science in China(Earth Sciences), 2016, 59(8):1597-1609. doi: 10.1007/s11430-015-0231-8
CrossRef Google Scholar
|
[7] |
周征宇, 廖宗廷, 袁媛, 等.青海软玉中"水线"的特征及其成因探讨[J].宝石和宝石学杂志, 2005, 7(3):10-12. doi: 10.3969/j.issn.1008-214X.2005.03.003
CrossRef Google Scholar
Zhou Z Y, Liao Z T, Yuan Y, et al.Study on characteristics and genesis of 'water line' in Qinghai nephrite jade[J]. Journal of Gems and Gemmology, 2005, 7(3):10-12. doi: 10.3969/j.issn.1008-214X.2005.03.003
CrossRef Google Scholar
|
[8] |
袁媛, 廖宗廷, 周征宇.青海软玉水线的物相分析和微观形貌研究[J].上海地质, 2005(4):68-70. doi: 10.3969/j.issn.2095-1329.2005.04.019
CrossRef Google Scholar
Yuan Y, Liao Z T, Zhou Z Y.Study on compositions and micro-textures of water-line in nephrite from Qinghai Province[J]. Shanghai Geology, 2005(4):68-70. doi: 10.3969/j.issn.2095-1329.2005.04.019
CrossRef Google Scholar
|
[9] |
刘虹靓, 杨明星, 杨天翔, 等.青海翠青玉的宝石学特征及颜色研究[J].宝石和宝石学杂志, 2013, 15(1):7-14. doi: 10.3969/j.issn.1008-214X.2013.01.002
CrossRef Google Scholar
Liu H L, Yang M X, Yang T X, et al.Study on colour and gemmological characteristics of viridis nephrite from Qinghai Province[J]. Journal of Gems and Gemmology, 2013, 15(1):7-14. doi: 10.3969/j.issn.1008-214X.2013.01.002
CrossRef Google Scholar
|
[10] |
Yu H Y, Wang R C, Guo J C, et al.Color-inducing elements and mechanisms in nephrites from Golmud, Qinghai, NW China:Insights from spectroscopic and compositional analyses[J]. Journal of Mineralogical & Petrological Sciences, 2016, 59:1597-1609.
Google Scholar
|
[11] |
Chen J B, Zeng Z G.Metasomatism of the peridotites from Southern Mariana fore-arc:Trace element characteristics of clinopyroxene and amphibole[J]. Science in China(Earth Sciences), 2007, 50(7):1005-1012. doi: 10.1007/s11430-007-0023-y
CrossRef Google Scholar
|
[12] |
Liu Y, Deng J, Shi G H, et al.Geochemistry and petrology of nephrite from Alamas, Xinjiang, NW China[J]. Journal of Asian Earth Sciences, 2011, 42(3):440-451. doi: 10.1016/j.jseaes.2011.05.012
CrossRef Google Scholar
|
[13] |
王汝成, 谢磊, 陈骏, 等.南岭中段花岗岩中榍石对锡成矿能力的指示意义[J].高校地质学报, 2011, 17(3):368-380. doi: 10.3969/j.issn.1006-7493.2011.03.002
CrossRef Google Scholar
Wang R C, Xie L, Chen J, et al.Titanite as an indicator mineral of tin mineralizing potential of granites in the Middle Nanling Range[J]. Geological Journal of China Universities, 2011, 17(3):368-380. doi: 10.3969/j.issn.1006-7493.2011.03.002
CrossRef Google Scholar
|
[14] |
赵文俞, 牟善斌, 秦麟卿, 等.木兰山蓝片岩中斜黝帘石-低铁绿帘石连生体的确定[J].岩矿测试, 2002, 21(1):29-32. doi: 10.3969/j.issn.0254-5357.2002.01.006
CrossRef Google Scholar
Zhao W Y, Mou S B, Qin L Q, et al.Determination of fine intergrowth of low-Fe epidote and clinoepidote in the glaucophane schist from Mulan mountain by electron probe microanalysis and optical microscopy[J]. Rock and Mineral Analysis, 2002, 21(1):29-32. doi: 10.3969/j.issn.0254-5357.2002.01.006
CrossRef Google Scholar
|
[15] |
Bocchio R, Diella V, Adamo I, et al.Mineralogical characterization of the gem-variety pink clinozoisite from Val Malenco, Central Alps, Italy[J]. Rendiconti Lincei, 2017, 28:1-9.
Google Scholar
|
[16] |
王永亚, 干福熹.广西陆川蛇纹石玉的岩相结构及成矿机理[J].岩矿测试, 2012, 31(5):788-793. doi: 10.3969/j.issn.0254-5357.2012.05.006
CrossRef Google Scholar
Wang Y Y, Gan F X.Mineral structure and mineralization mechanism of serpentine jade from Luchuan, Guangxi Province[J]. Rock and Mineral Analysis, 2012, 31(5):788-793. doi: 10.3969/j.issn.0254-5357.2012.05.006
CrossRef Google Scholar
|
[17] |
吕书君, 杨富全, 柴凤梅, 等.新疆准噶尔北缘托斯巴斯套铁铜金矿床矽卡岩和磁铁矿矿物学特征及其地质意义[J].岩矿测试, 2013, 32(3):510-521. doi: 10.3969/j.issn.0254-5357.2013.03.027
CrossRef Google Scholar
Lü S J, Yang F Q, Chai F M, et al.Mineralogical characteristics of skarn in Tuosibasitao iron-copper-gold deposits of the northern margin of Junggar, Xinjiang, and their geological significance[J]. Rock and Mineral Analysis, 2013, 32(3):510-521. doi: 10.3969/j.issn.0254-5357.2013.03.027
CrossRef Google Scholar
|
[18] |
Lacroix B, Charpentier D, Buatier M, et al.Formation of chlorite during thrust fault reactivation.Record of fluid origin and P-T conditions in the Monte Perdido thrust fault (Southern Pyrenees)[J]. Contributions to Mineralogy & Petrology, 2012, 163(6):1083-1102.
Google Scholar
|
[19] |
李立兴, 朱明玉, 方同明, 等.应用电子探针技术研究北京密云放马峪铬铁矿床成因-来自含铬尖晶石矿物化学的证据[J].岩矿测试, 2015, 34(5):600-608.
Google Scholar
Li L X, Zhu M Y, Fang T M, et al.Origin of the Fangmayu chromite deposit, Miyun, Beijing:Constraints from electron microprobe analyses of Cr-spinel[J]. Rock and Mineral Analysis, 2015, 34(5):600-608.
Google Scholar
|
[20] |
包鲁明, 谭劲, 池召坤, 等.透辉石-钙长石体系熔体在不同过冷条件下晶体生长研究[J].矿物岩石, 2009, 29(3):17-22. doi: 10.3969/j.issn.1001-6872.2009.03.004
CrossRef Google Scholar
Bao L M, Tan J, Chi Z K, et al.Crystal growth of diopside-anorthite melting system under different undercooking condition[J]. Acta Petrological and Mineralogical, 2009, 29(3):17-22. doi: 10.3969/j.issn.1001-6872.2009.03.004
CrossRef Google Scholar
|
[21] |
Gottschalk M, Andrut M, Melzer S.The determination of the cummingtonite content of synthetic tremolite[J]. European Journal of Mineralogy, 1999, 11(11):967-982.
Google Scholar
|
[22] |
Paolo B, Giovanni B A, Girolamo B.Crystal chemical and structural characterization of fibrous tremolite from Susa Valley, Italy, with comments on potential harmful effects on human health[J]. American Mineralogist, 2008, 93(8-9):1349-1355. doi: 10.2138/am.2008.2869
CrossRef Google Scholar
|
[23] |
梁祥济.中国矽卡岩和矽卡岩矿床形成机理的实验研究[M].北京:学苑出版社, 2000:152-186.
Google Scholar
Liang X J.Experimntal Studies on the Mechanism of the Formation of Skarns and Skarn Ore Deposits in China[M]. Beijing:Academy Press, 2000:152-186.
Google Scholar
|
[24] |
何明跃, 王濮.石英的结晶度指数及其标型意义[J].矿物岩石, 1994, 14(3):22-28.
Google Scholar
He M Y, Wang P.The crystallinity of quartz and its typomorphic significance[J]. Minerals and Rocks, 1994, 14(3):22-28.
Google Scholar
|