稀土元素分布在迪特劳河流沉积物中的分布 性大山,东卡尔巴提亚山脉
Valentin Nicolae Coțac1, Ovidiu Gabriel Iancu1, Nicușor Necula1,2
1Department of Geology, Faculty of Geography and Geology, Alexandru Ioan Cuza University of Iasi, Iași, Romania.
PloS one
|December 5, 2024
概括
罗马尼亚的河流沉积物.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 石化学 石化学是一门学科.
背景情况:
- 罗马尼亚的迪特劳性山脉在地质上是独一无二的,有着各种各样的岩石类型.
- 过去的采矿勘探表明有价值的矿产矿床的潜力.
- 了解沉积物组成是评估资源潜力的关键.
研究的目的:
- 分析Ditrău和Jolotca河流沉积物的地化学组成.
- 量化稀土元素 (REE) 和微量元素度.
- 确定矿物质特征和元素的潜在来源.
主要方法:
- 感应合等离子体质谱 (ICP-MS) 用于元素分析.
- 粉末X射线衍光度和电子显微镜用于矿物识别.
- 从Ditrău和Jolotca河流的河床沉积物的分析.
主要成果:
- 在沉积物中发现的高度的轻稀土元素 (LREEs),特别是和兰.
- 丰富的微量元素,如,和.
- 识别含有REE的矿物质,如莫纳和埃皮多特.
- 不同的矿物组合 (石英,K Feldspar,阿尔比特) 和二氧化/石灰的存在表明各种来源.
结论:
- 迪特劳河和约洛特卡河的沉积物富含可再生能源和微量元素.
- 矿物学分析证实了有价值的重矿物的存在.
- 地化学特征表明,Ditrau的来源是混合的基/基础,Jolotca的来源是酸性.
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