内蒙古阿钦楚鲁二长花岗岩锆石SHRIMP U-Pb年龄及地球化学特征

doi:10.13278/j.cnki.jjuese.201501114

Abstract

Abstract:

The Achieng Qulu monzogranite complex is located in the middle of Early Paleozoic Chaganaobao-Aoyoute-Chaobuleng tectonic-magmatic belt which belongs to the southeast margin of the Siberian plate. The main rock types of the complex are moderate-and fine-grained monzogranite as well as moderate-and coarse-grained monzogranite. SHRIMP zircon U-Pb isotopic dating result indicates that the emplacement age of Achieng Qulu monzogranite is (296.3±3. 8) Ma, namely Late Hercynian. Rock geochemical analysis shows silicon-rich of the monzogranite, as peraluminous with SiO₂ content of 73.48% to 74.22%;with Al₂O₃ content of 13.63% to 14.01% and A/CNK ratio of 1.04 to 1.10;alkali-rich, (K₂O+Na₂O) content of 8.08% to 8.54%, with Rittmann index of (σ) 2.13 to 2.46, relatively rich in potassium, K₂O/Na₂O ratio of 1.31 to 1.54, belonging to high-K calc-alkaline series;enriched in such large ion lithophile elements as Rb, Sr, Ba and light rare earth elements (LREE), relatively depleted in high field strength elements such as Ta, Nb, Ti;total REE to 112.05×10^-6-130.16×10^-6, moderate negative Eu anomality (δEu=0.52 to 0.65), showing a slightly rightward with steep LREE line and slow HREE line, containing geochemical characteristics of from post-collision high-K granite to A-type granites. Relatively low initial ⁸⁷Sr/⁸⁶Sr ratios (0.703 849 to 0.704 236) and positive ε_Nd(t) values (4.2 to 4.3), reflect that the material source of the complex may be mainly derived from the new continental crust formed by underplating of mantle-derived magma. Based on the data mentioned above and discrimination on tectonic setting, combined with regional comparison, we conclude that the Achieng Qulu monzogranite belongs to post-collision high-K calc-alkaline granite derived from the partial melting of the upper crust, which is caused by sub-ducted slab break-off, asthenosphere upwelling and partial melting of the lithosphere mantle, meanwhile, part of the mantle-derived magma under-plated to the lower part of the crust or formed mafic intrusions invading crust. These events took place under the dynamics background of lithosphere transforming from compressive thickening to extension system. This recognition provides petrology evidence and age restricting for the Late Paleozoic tectonic magmatic evolution of East Wuzhu Muqinqi and for post-orogenic extensional tectonic mechanism transformation from geochemical combination after the collision against Siberian plate and the North China plate.

Key words: monzogranite, SHRIMP zircon U-Pb age, geochemistry, post-collision, Inner Mongolia, Achieng Qulu

CLC Number:

P588.121

Wang Zhihua, Chang Chunjiao, Cong Runxiang, Wang Liang, Ma Dexi, Wang Xiaojun. SHRIMP Zircon U-Pb Age and Geochemical Characteristics of the Achieng Qulu Monzogranite in Inner Mongolia[J].Journal of Jilin University(Earth Science Edition), 2015, 45(1): 166-187.

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SHRIMP Zircon U-Pb Age and Geochemical Characteristics of the Achieng Qulu Monzogranite in Inner Mongolia

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