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DOI | 10.1111/1755-6724.14919 |
Rutile to Titanite Transformation in Eclogites and its Geochemical Consequences: An Example from the Sumdo Eclogite, Tibet | |
Zhao, Linghao; Zeng, Lingsen; Gao, Li'e; Hu, Mingyue; Sun, Dongyang; Zhang, Lifei | |
发表日期 | 2023 |
ISSN | 1000-9515 |
EISSN | 1755-6724 |
起始页码 | 122 |
结束页码 | 133 |
卷号 | 97期号:1 |
英文摘要 | The formation of titanite coronae after rutile is common in retrograde high- to ultrahigh-pressure meta-mafic rocks, which provides a good opportunity to address the geochemical behavior of HFSE in crustal environments. In the Sumdo eclogite, titanite occurs either as a corona around rutile grains or as semi-continuous veins cross-cutting the major foliation, whereas rutile grains occur either as inclusions in garnet or omphacite or as a relict core surrounded by titanite. Textural relationships and trace elements characteristics of rutile and titanite with different occurrences indicate that both minerals preferentially incorporate Nb and Hf over Ta and Zr in aqueous fluid. Moreover, the breakdown of omphacite and epidote could release substantial amounts of aqueous fluids enriched in Ca, Si, Fe and REE, which would react with rutile to form titanite coronae and veins. During this process, water-insoluble elements, like HFSE and HREE, behave like mobile elements, but they do not migrate substantially out of the system, instead, tending to react in situ. This suggests that the aqueous fluids released during the retrograde metamorphic reactions in mafic rocks could not substantially transfer fluid-immobile elements into the overlying mantle wedge in subduction environments. |
关键词 | Sumdo eclogiterutiletitanitetrace element geochemistryNb-Ta fractionation |
英文关键词 | BEARING AQUEOUS FLUIDS; TRACE-ELEMENTS; SUBDUCTION-ZONES; HIGH-PRESSURE; EXPERIMENTAL CONSTRAINTS; ZIRCON GEOCHRONOLOGY; NB/TA FRACTIONATION; CONTINENTAL-CRUST; ION MICROPROBE; LHASA TERRANE |
WOS研究方向 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000952820100008 |
来源期刊 | ACTA GEOLOGICA SINICA-ENGLISH EDITION |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/283483 |
作者单位 | Ministry of Natural Resources of the People's Republic of China; China Geological Survey; Chinese Academy of Geological Sciences; Institute of Geology, Chinese Academy of Geological Sciences; Peking University |
推荐引用方式 GB/T 7714 | Zhao, Linghao,Zeng, Lingsen,Gao, Li'e,et al. Rutile to Titanite Transformation in Eclogites and its Geochemical Consequences: An Example from the Sumdo Eclogite, Tibet[J],2023,97(1). |
APA | Zhao, Linghao,Zeng, Lingsen,Gao, Li'e,Hu, Mingyue,Sun, Dongyang,&Zhang, Lifei.(2023).Rutile to Titanite Transformation in Eclogites and its Geochemical Consequences: An Example from the Sumdo Eclogite, Tibet.ACTA GEOLOGICA SINICA-ENGLISH EDITION,97(1). |
MLA | Zhao, Linghao,et al."Rutile to Titanite Transformation in Eclogites and its Geochemical Consequences: An Example from the Sumdo Eclogite, Tibet".ACTA GEOLOGICA SINICA-ENGLISH EDITION 97.1(2023). |
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