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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 被引量:7
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作者 华献武 胡瑞忠 D.H.Cornell 《科学通报》 EI CAS CSCD 北大核心 2000年第13期1429-1432,共4页
运用激光熔样ICP-MS技术,测定了云南省姚安金矿区矿化蚀变带中原生条纹长石及相应蚀变产物次生钾长石的稀土元素(REE)组成.相对于原生条纹长石,次生钾长石具有较高的REE含量和较小的正 Eu异常,但两者的 REE模式... 运用激光熔样ICP-MS技术,测定了云南省姚安金矿区矿化蚀变带中原生条纹长石及相应蚀变产物次生钾长石的稀土元素(REE)组成.相对于原生条纹长石,次生钾长石具有较高的REE含量和较小的正 Eu异常,但两者的 REE模式类似.这些特征表明,造成本区矿化蚀变带中高 REE含量次生钾长石的流体,应为富碱侵入岩成岩过程中分异出的富含REE的岩浆流体. 展开更多
关键词 原生长石 次生长石 蚀变流动 矿化 稀土
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Soil Erosion Changes over the Past Five Decades in the Red Soil Region of Southern China 被引量:18
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作者 LIANG Yin LI Decheng +5 位作者 LU Xixi YANG Xuan PAN Xianzhang MU Huan SHI Deming ZHANG Bin 《Journal of Mountain Science》 SCIE CSCD 2010年第1期92-99,共8页
This paper reports the dynamic changes of soil and water loss in the red soil region of Southern China since the 1950s. The red soil region covers eight provinces: Jiangxi, Zhejiang, Fujian, Anhui, Hubei, Hunan, Guang... This paper reports the dynamic changes of soil and water loss in the red soil region of Southern China since the 1950s. The red soil region covers eight provinces: Jiangxi, Zhejiang, Fujian, Anhui, Hubei, Hunan, Guangdong and Hainan. From the 1950s to 1986, the annual rate of soil erosion increased by 3.4%. From 1986 to 1996 and from 1996 to 2000, the annual rates of soil erosion decreased by 2.0% and 0.32%, respectively. Field surveys showed that from 2000 to 2005, the area of soil and water loss decreased annually by 1.2%. This decrease was a result of large-scale erosion control activities across China. Although the eroded soil has been restored, the restoration process is very slow and full restoration will take a long time. Our report suggests that controlling soil and water loss is a challenging task, and additional measures must be taken to effectively control the soil erosion in the red soil region. 展开更多
关键词 red soil region soil and water loss dynamic change remote sensing field samplingsurvey
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