Arid
DOI10.1016/j.jseaes.2021.104773
Geochemistry and origin of high-Sr carbonatite from the Nuba Mountains, Arabian-Nubian Shield, Sudan
Baioumy, Hassan
通讯作者Baioumy, H (corresponding author), Cent Met R&D Inst, Minerals Technol Div, POB 87, Cairo, Egypt.
来源期刊JOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
EISSN1878-5786
出版年2021
卷号214
英文摘要Carbonatite from the Arabian-Nubian Shield of Sudan occurs as dykes in the Nuba Mountains. It is composed of calcite with some feldspars, quartz and fluorite. CaO is the major constituent in this carbonatite and accordingly, it is classified as calico-carbonatite. The studied carbonatite shows exceptionally high concentrations of SrO (4.4 to 5.9 wt%). Ba, Pb and Y occur in relatively higher concentrations compared to other trace elements. Concentration of rare earth elements (sigma REEs) is relatively low (average 1550 ppm) compared to many primary igneous carbonatites. The chondrite-normalized REE patterns display higher light rare earth elements (LREEs) compared to heavy rare earth elements (HREEs) with slight negative Ce/Ce* and Eu/Eu* anomalies. The 818OVSMOW values range between 7.48 and 10.05 & permil;, while 813CV-PDB values vary from -6.24 to - 7.38 & permil;, which is close to the primary carbonatites values. Occurrence of carbonatite as dykes with cumulate and triple junction textures, plot of the carbonatite in the true carbonatite fields of the Ba-Sr and Ba + Sr-REE + Y diagrams, igneous-derived 813CV-PDB and 818OV-SMOW values and high (La/Yb)N ratios indicate its primary igneous origin. The strong positive correlation between REEs and Sr suggests the occurrence of these elements as secondary strontianite, which was confirmed by SEM and EDX analyses. This might indicate that the enrichment of REEs and Sr in the studied carbonatite is not from the primary magma and most probably took place during a sub-solidus metasomatic process after the carbonatite emplacement.
英文关键词Carbonatite Arabian-Nubian Shield Nuba Mountains Sudan REE Strontium Stable isotopes Origin
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000656155900003
WOS关键词EASTERN DESERT ; COMPLEX ; PETROGENESIS ; ISOTOPE ; GENESIS ; MANTLE ; PARAGENESIS ; MINERALOGY ; ELEMENTS ; GRAVITY
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/350733
作者单位[Baioumy, Hassan] Cent Met R&D Inst, Minerals Technol Div, POB 87, Cairo, Egypt
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Baioumy, Hassan. Geochemistry and origin of high-Sr carbonatite from the Nuba Mountains, Arabian-Nubian Shield, Sudan[J],2021,214.
APA Baioumy, Hassan.(2021).Geochemistry and origin of high-Sr carbonatite from the Nuba Mountains, Arabian-Nubian Shield, Sudan.JOURNAL OF ASIAN EARTH SCIENCES,214.
MLA Baioumy, Hassan."Geochemistry and origin of high-Sr carbonatite from the Nuba Mountains, Arabian-Nubian Shield, Sudan".JOURNAL OF ASIAN EARTH SCIENCES 214(2021).
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