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- W3149936716 abstract "Muchang 合成侵入被定位 Fengwei 镇和 Baoshan-Zhenkang 块的南方的大约 14 km 东南。裂缝相关的侵入在东方和西方由早阶段的 riebeckite nordmarkite 组成方面和不连续的边缘的地区，主导的 riebeckite 花岗石的迟了阶段的主要身体，和次要的 aegirine 花岗石。petrological 地球化学和在花岗石和联系 skarn 类型 Luziyuan Pb-Zn 存款之间的 Muchang 碱花岗石和关系的迟了阶段的 riebeckite 花岗石，起源和进化标明日期的 LA-ICP-MS 锆石 U-Pb 上的研究在这份报纸被讨论。结果证明 Muchang 碱花岗石属于 A 类型花岗石，它被丰富在 Al2O3， SiO2，全部的碱和 Fe 描绘，在有高 FeOT/MgO 比率的 MgO 和 CaO 内容的弄空。REE 集中相对高，高度展出 fractionated LREE 模式与显著地 Eu 否定异例。Muchang 花岗石显然在亲石元素元素被充实(例如， Rb， K， U 和 Th ) 并且高领域力量元素(例如， Zr， Hf， Nb， Y 和 Ga ) 与高度 10000" @default.
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- W3149936716 date "2010-01-01" @default.
- W3149936716 modified "2023-09-23" @default.
- W3149936716 title "LA-ICP-MS Zircon U-Pb Geochronology and Petrology of the Muchang Alkali Granite,Zhenkang County,Western Yunnan Province,China" @default.
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