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中国科学院地球化学研究所机构知识库
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矿床地球化学国家重点... [5]
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Petrogenesis of skarn in Shizhuyuan W-polymetallic deposit, southern Hunan, China: Constraints from petrology, mineralogy and geochemistry
期刊论文
Transactions of Nonferrous Metals Society of China, 2016, 卷号: 26, 期号: 6, 页码: 1676-1687
Authors:
Yong-sheng CHENG
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Submit date:2017/11/20
S-Pb isotopic geochemistry of Xiuwacu magmatic hydrothermal Mo-W deposit in Zhongdian area, NW Yunnan: Constrains on the sources of metal
期刊论文
岩石学报, 2015, 卷号: 31, 期号: 11, 页码: 3171-3188
Authors:
Wang XS(王新松)
;
Bi XW(毕献武)
;
Hu RZ(胡瑞忠)
;
Leng CB(冷成彪)
;
Yu HJ(余海军)
;
Yin GH(尹光侯)
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Submit date:2017/05/18
Fluid inclusion and mineralization of Dafulou tin deposit in Dachang metal district, Guangxi, south China
期刊论文
Transactions of Nonferrous Metals Society of China, 2013, 卷号: 23, 期号: 9, 页码: 2726-2735
Authors:
Cheng Yong-sheng
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Submit date:2014/05/13
Fluid Inclusion
Mineralization
Sn-polymetallic Deposit
Dafulou
Dachang
花岗岩化学风化过程中的Sr同位素演化──矿物相对风化速率的影响
期刊论文
中国科学(D辑:地球科学), 2001, 期号: 8, 页码: 634-640
Authors:
马英军
;
刘丛强
Adobe PDF(416Kb)
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Submit date:2018/02/27
锶同位素
化学风化
风化速率
非化学计量性
花岗岩
山西吕梁山界河口群变质基性火山岩的地球化学及年代学研究
期刊论文
中国科学(D辑:地球科学), 2001, 期号: 2
Authors:
刘建忠
;
张福勤
;
欧阳自远
;
李春来
;
邹永廖
;
徐琳
Adobe PDF(442Kb)
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Submit date:2017/05/24
蚀变流体的来源:矿化蚀变带中原生与次生长石的稀土元素证据
期刊论文
科学通报, 2000, 卷号: 45, 期号: 13, 页码: 1429-1432
Authors:
毕献武
;
Corn.,DH
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Submit date:2014/04/17
原生长石
次生长石
蚀变流动
矿化蚀变带
稀土
白云岩风化剖面的元素地球化学特征及其对上陆壳平均化学组成的意义——以黔北新蒲剖面为例
期刊论文
中国科学(D辑:地球科学), 1999, 期号: 6
Authors:
季宏兵
;
欧阳自远
;
王世杰
;
周德全
Adobe PDF(310Kb)
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Submit date:2016/03/10
风化剖面
元素地球化学
平均上陆壳化学组成
白云岩