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Petrology and Geochemistry of Granitoid from South Sulawesi, Indonesia: Implication for Rare Earth Element (REE) Occurrences

机译:印度尼西亚南苏拉威西岛花岗岩类的岩石学和地球化学:对稀土元素(REE)赋存的影响

摘要

This study reports petrology and geochemistry of potential rare earth elements (REE) bearing granitoid from South Sulawesi. The granitoid consists of monzogranite, granodiorite and diorite with subordinate of quartz monzonite, monzodiorite and syenite. Major and trace element analysis were determined using XRF method while trace element and rare earth element composition were determined by ICP-MS method. Geochemical study suggested that the granitoid were metaluminous series and ???I-type??? granitoid. They were furthered classified as calc alkaline series in AFM diagram. The total REE concentration in the granitoids range from 279 ppm to 400 ppm whereas total REE + Y contents up to 305 ppm for Polewali and 428 ppm for Masamba granitoid.udChondrite normalized REE patterns were characterized by enrichment of LREE with the depletion of heavy HREE. REE-bearing mineral were detected as zircon, apatite and monazite as shown by the positive correlation between Zr and P2O5 contents in bulk rock with REE content.
机译:这项研究报告了南苏拉威西岛含花岗岩的潜在稀土元素(REE)的岩石学和地球化学。花岗岩类由辉长花岗岩,花岗闪长岩和闪长岩组成,其次为石英辉长岩,单闪长岩和正长岩。用XRF法测定主要和痕量元素,用ICP-MS法测定痕量元素和稀土元素。地球化学研究表明,该类花岗岩为金属系列和“ I型”。花岗岩。在AFM图中将它们进一步分类为钙碱性系列。花岗岩中的总REE浓度范围为279 ppm至400 ppm,而Polewali的总REE + Y含量高达305 ppm,Masamba花岗岩的总REE含量高达428 ppm。 。锆和磷灰石含量与稀土元素含量呈正相关,表明含稀土元素的矿物为锆石,磷灰石和独居石。

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