Zircon U-Pb age of Baiyingaolao Formation dacite in Chaganchulute of Zhalute Banner, Inner Mongolia
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图 1 研究区地质简图(a)、英安岩正交偏光显微照片(b)及LA-MC-ICP-MS锆石U-Pb年龄谐和图(c)
Qh—第四系全新统;K1ml—下白垩统梅勒图组;K1b—下白垩统白音高老组;J3mn—上侏罗统玛尼吐组;J3mk—上侏罗统满克头鄂博组;P1ŝŝ —下二叠统寿山沟组;ξγK1—早白垩世正长花岗岩;νK1—早白垩世辉长岩;▲—同位素年龄采样点、年龄值及编号;Qz−石英;Pl−斜长石;Bi−黑云母
Figure 1. Geological map of the study area (a), orthogonally polarized micrograph of dacite and LA-MC-ICP-MS zircon U-Pb concordia plots
Qh-Quaternary Holocene series; K1ml—Lower Cretaceous Meiletu Formation; K1b—Lower Cretaceous Baiyingaolao Formation; J3mn−Upper Jurassic Manitu Formation; J3mk−Upper Jurassic Manketouebo Formation; P1ŝŝ−Lower Permian Shoushangou Formation; ξγK1—Early Cretaceous syenogranite; νK1—Early Cretaceous gabbro; ▲—Isotopic age sampling position, age value and number; Qz-quartz; Pl-plagioclase; Bi-Biotite
表 1 内蒙古扎鲁特旗查干楚鲁特白音高老组英安岩锆石U-Pb分析结果
Table 1 LA-MC-ICP-MS U-Pb data of the zircons from Baiyingaolao Formation Dacite in the Chaganchulute of zhaluteqi, Inner Mongolia