Application of X-ray photoelectron spectroscopy in mineral deposit studies
Application of X-ray photoelectron spectroscopy in mineral deposit studies
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X射线光电子能谱在矿床研究中的应用
DOI:
10.1080/03717453.2017.1306294
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发表时间:
2017
期刊:
影响因子:
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通讯作者:
Smith M
中科院分区:
文献类型:
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作者:
Smith M
Mineral deposits associated with silica-undersaturated, nepheline syenites are an important source of critical metals, such as the rare earth elements (REE) and niobium, and a number of other commodities (eg phosphorus, titanium and zircon). In particular, it is highly-peralkaline, or hyperagpaitic nepheline syenites that are typically associated with economic concentrations of Nb, REE, Zr and Ti (eg Ilímaussaq in Greenland). However, miaskitic nepheline syenites contain much lower concentrations of these elements and are typically not economically mineralised. Therefore mineralised examples of miaskitic rocks, such as the Ditrãu Alkaline Igneous Complex (DAIC) in Romania, are of real interest because they further diversify the REE supply base, thus reducing potential risk to supply.The Triassic DAIC is a miaskitic nepheline syenite body in north-eastern Romania. The ring-shaped intrusion is tilted and covers an area of approximately 200 km (Lenz et al. 2013). To the north-west it comprises a series of amphibolites, and alkali diorites and gabbros, with syenites, nepheline syenites and alkali granites cropping out in the east. The eastern margin comprises hydrothermally altered nepheline syenite that is considered to represent the roof-zone of the complex (Honour 2015). The complex is cut by a series of mineralised veins that contain predominantly monazite and allanite in a carbonate and Sulfide gangue. Previous work has largely focused on the age and petrogenesis of the complex and the mineralogy of the associated mineralisation. However, attempts to
DOI:
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发表时间:
2000
期刊:
影响因子:
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作者:
K. Kaltoft;D. Schlatter;L. Kludt
通讯作者:
L. Kludt