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DOI | 10.1016/j.oregeorev.2019.103031 |
Geochronology, geochemistry and Sr-Nd-Hf isotopic compositions of Late Cretaceous-Eocene granites in southern Myanmar: Petrogenetic, tectonic and metallogenic implications | |
Li, Jin-Xiang; Fan, Wei-Ming; Zhang, Li-Yun; Evans, Noreen J.; Sun, Ya-Li; Ding, Lin; Guan, Qiu-Yun; Peng, Tou-Ping; Cai, Fu-Long; Sein, Kyaing | |
通讯作者 | Li, JX (通讯作者) |
发表日期 | 2019 |
ISSN | 0169-1368 |
EISSN | 1872-7360 |
卷号 | 112 |
英文摘要 | The geochronology, petrogenesis and tectonic setting of granites associated with tin-tungsten mineralization in southern Myanmar remain unclear. This work presents whole-rock geochemical, Sr-Nd isotopic, and zircon U-Pb and Hf isotopic data for felsic intrusions in the Sibusima terrane. Zircon U-Pb dating indicates formation in the Late Cretaceous-Early Eocene (similar to 84-48 Ma) and suggests that these intrusions likely represent a southward extension of the coeval magmatic belt in the Tengchong terrane. Primarily classified as high-K talc-alkaline, the granites show strong enrichments in large ion lithophile elements (e.g., Cs, Rb, and K), depletions in Nb, Ta, P, and Ti, and negative Ba and Sr anomalies on primitive mantle-normalized diagrams. P2O5, CaO, Al2O3, MgO, TiO2 contents, and Nb/Ta ratios decrease with increasing SiO2 contents, possibly consistent with evolution trends in fractionated l-type granitic magmas. In addition, these intrusions display a wide range of negative epsilon(Nd)(t) (-14.6--.5.5) and zircon epsilon(Hf)(t) values (-22.7-5.7), suggesting a dominant Sibusimacrustal source with a minor mantle contribution. Notably, the Eocene and a few Paleocene granites show more contribution of mantle material based on higher epsilon(Nd)(t) (-8.5--5.5) and zircon epsilon(Hf)(t) (-11.0--3.2) values. Large variations in zircon Hf isotopic compositions within an individual Eocene granitic intrusion (e.g.,-15.2-5.7) and corresponding biotite-rich enclave (-17.8-0.2) likely indicate magma mixing. Considering the spatial-temporal distribution of magmatism in the West Burma and Sibusima terranes, the studied Late Cretaceous-Eocene felsic magmas likely formed in a continental arc setting during normal subduction (similar to 100-60 Ma) and subsequent roll-back of the Neo-Tethyan oceanic lithosphere (similar to 60-50 Ma). Additionally, most of granites have the elevated Sn with increasing Rb/Sr ratios, and decreasing TiO2 contents and Nb/Ta ratios, suggesting Sn enrichment is primarily controlled by magmatic fractionation. Meanwhile, Sn and Li depletions in some granites deviate from the magmatic evolution trend, likely as a result of fluid exsolution. The exsolved Sn-rich fluids could have made a genetic contribution to hydrothermal Sn mineralization in southern Myanmar. |
关键词 | ZIRCON U-PBA-TYPE GRANITESI-TYPE GRANITESSN-W DEPOSITO ISOTOPESTIN BELTLU-HFNEOTETHYAN SUBDUCTIONMALAYSIAN GRANITOIDSTENGCHONG BLOCK |
英文关键词 | Late Cretaceous-Eocene; Granite; Roll-back; Tin metallogeny; Myanmar |
语种 | 英语 |
WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
WOS类目 | Geology ; Mineralogy ; Mining & Mineral Processing |
WOS记录号 | WOS:000487168100043 |
来源期刊 | ORE GEOLOGY REVIEWS |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259578 |
推荐引用方式 GB/T 7714 | Li, Jin-Xiang,Fan, Wei-Ming,Zhang, Li-Yun,et al. Geochronology, geochemistry and Sr-Nd-Hf isotopic compositions of Late Cretaceous-Eocene granites in southern Myanmar: Petrogenetic, tectonic and metallogenic implications[J]. 中国科学院青藏高原研究所,2019,112. |
APA | Li, Jin-Xiang.,Fan, Wei-Ming.,Zhang, Li-Yun.,Evans, Noreen J..,Sun, Ya-Li.,...&Sein, Kyaing.(2019).Geochronology, geochemistry and Sr-Nd-Hf isotopic compositions of Late Cretaceous-Eocene granites in southern Myanmar: Petrogenetic, tectonic and metallogenic implications.ORE GEOLOGY REVIEWS,112. |
MLA | Li, Jin-Xiang,et al."Geochronology, geochemistry and Sr-Nd-Hf isotopic compositions of Late Cretaceous-Eocene granites in southern Myanmar: Petrogenetic, tectonic and metallogenic implications".ORE GEOLOGY REVIEWS 112(2019). |
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