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您的检索式：作者名="R.N.Wilson"
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| 1 | 白云鄂博稀土氟碳酸盐矿物的共面网定向附生结构显示文摘首次在白云鄂博碳酸岩岩墙中发现了氟碳铈矿和氟碳钙铈矿等稀土氟碳酸盐矿物 ,并运用偏光显微镜、阴极发光、扫描电子显微镜和电子探针等手段对其进行了观察和分析 .研究表明 ,氟碳铈矿很少呈单一均匀晶体存在 ,多含有氟碳钙铈矿微细客晶 ,沿 (0 0 1)面网与其构成规则的共面网定向附生结构 (epitaxy) .氟碳钙铈矿也含有氟碳铈矿微细客晶 ,它们形成规则的面衍生结构 .这种面衍生结构是矿物因结晶介质的化学成分变化所引起的 。 | 杨学明 张培善 陶克捷 杨晓勇 陈双喜 邹明龙 M.J.LeBas R.N.Wilson R.Branson L.S.Campbell T.C.Williams P.Henderson | 1998 | 科学通报1998，43，2： | 7 |
| 2 | 白云鄂博钡稀土氟碳酸盐矿物的新产状及其矿物学特征显示文摘对产于白云鄂博碳酸岩岩墙中的钡稀土氟碳酸盐矿物的化学成分、稀土配分和连生关系作了研究 ,观察到了氟碳铈钡矿与氟碳钡铈矿、以及氟碳钡铈矿和黄河矿的体衍生构造(syntaxy) .它们直接形成于碳酸岩浆的结晶作用 .这些矿物的稀土配分型式与矿床赋矿白云石大理岩中的相应矿物十分相似 ,暗示其有成因上的联系 . | 杨学明 杨晓勇 陈双喜 陈天虎 张培善 陶克捷 M.J.LeBas R.N.Wilson R.Branson L.S.Campbell T.C.Williams P.Henderson | 1999 | 科学通报1999，44，9： | 7 |
| 3 | New occurrence of Ba-REE fluorcarbonate minerals at Bayan Obo,Inner Mongolia,North China,and their mineralogical features显示文摘Ba-REE fluorcarbonate minerals from a carbonatite dyke at Bayan Obo, Inner Mongolia, North China, are first reported in this contribution, in which chemical composition, rare earth element (REE) patterns, and intergrowth relationships for these minerals have been investigated. Syntactic intergrowth or syntaxy between cebaite and cordylite, as well as cordylite and huanghoite were observed. This syntactic texture resulted from the variation of chemical composition of crystallizing agents for those minerals that crystallized directly from carbonatite magmas. It is worth noting that REE patterns of the Ba-REE fluorcarbonate minerals in the dyke are similar to those of the corresponding minerals from the ore hosted dolomite marble of the Bayan Obo giant REE-Nb-Fe mineral deposit, which implies their relation in origin. | M.J.Le Bas R.N.Wilson R.Branson L.S.Campbell T.C.Williams P.Henderson | 1999 | Chinese Science Bulletin1999，44，15： | 1 |
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