内蒙东部晚古生代构造格局:来自中、晚二叠-早三叠世砂岩碎屑锆石U-Pb年代学的证据
Late Paleozoic tectonic framework of eastern Inner Mongolia: Evidence from the detrital zircon U-Pb ages of the Mid-late Permian to Early Triassic sandstones
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摘要: 内蒙东部的克旗-林西-阿鲁科尔沁-扎鲁特-索伦-蘑菇气地区位于华北板块与西伯利亚板块所夹持的中亚造山带东段，西拉木伦缝合带与贺根山-黑河缝合带之间，是古亚洲洋晚古生代残余海盆最后消失的地区，保存了上述两缝合带构造演化过程的相关信息。本文针对中、晚二叠-早三叠世砂岩开展碎屑锆石LA-ICP-MS U-Pb年代学研究。测试的上二叠统林西组与下三叠统陶海营子组、老龙头组砂岩均具有成分成熟度低，近源快速沉积的特点，碎屑骨架成分显示多为火山岩区物源供给。锆石CL图和Th/U值也指示了绝大多数锆石为岩浆成因锆石。结合前人研究成果，区域内已获得的2533粒碎屑锆石U-Pb年龄主要分为3组：约230~570Ma （峰值年龄为270~315Ma、430Ma和500Ma）、700~1100Ma（峰值970Ma）及>1500Ma（峰值1800Ma和2500Ma）。较古老的峰值年龄1800Ma和2500Ma，暗示了华北克拉通基底的物源信息。其余两组年龄则与西拉木伦缝合带北侧的额尔古纳-兴安-锡林浩特地块内部岩浆事件的时间相吻合。对比分析内蒙东部不同区域（克旗-林西地区、阿鲁科尔沁-扎鲁特地区和索伦-蘑菇气地区）、不同时代（中、晚二叠世-早三叠世）沉积物碎屑组分变化趋势，推测古亚洲洋最终沿西拉木伦缝合带自西向东呈“剪刀”式闭合，时间持续至早三叠世。此外，索伦-蘑菇气地区中、晚二叠-早三叠世相对稳定的物源供给，证实了额尔古纳-兴安地块与松辽-锡林浩特地块至少在中二叠世沉积以前就已经沿贺根山-黑河缝合带完成拼贴，应为前人提出的早石炭世末。
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关键词:
- 内蒙东部 /
- 中亚造山带 /
- 中、晚二叠-早三叠世 /
- 碎屑锆石U-Pb年龄 /
- 构造格局
Abstract: The studied Hexigten Banner-Lixin-Ar Horqin Banner-Jarud Banner-Suolun-Moguqi areas in eastern Inner Mongolia, tectonically locate between the Xar Moron suture zone and the Hegenshan-Heihe suture zone, and belong to the eastern segment of the Central Asian Orogenic Belt (CAOB) between the North China and Siberia cratons. These areas significantly preserved records related to the Late Paleozoic closure of the Paleo-Asian Ocean, as well as the information of tectonic evolution of the Xar Moron suture and the Hegenshan-Heihe suture. This study focuses on the researches of detrital zircon LA-ICP-MS U-Pb ages of the Mid-late Permian to Early Triassic sandstones derived from the above mentioned areas. Petrologically, the detrital compositions indicate that the investigated sandstones are immature, probably due to the results of rapid erosion, transport, and diagenetic process and nearly supplying derived from the source. Additionally, the abundance of volcanic lithic significantly reveals the magmatic provenance mainly dominated. Meanwhile, the cathodoluminescence (CL) images of analyzed zircons and their Th/U ratios also imply the igneous origin. By combining our new geochronological data with previously reported data, total 2533 detrital zircon U-Pb ages are compiled and show three distinct dominant populations of ca. 230~570Ma (peak at ca.270~315Ma, 430Ma and 500Ma), ca.700~1100Ma (peak at 970Ma) and >1500Ma (peak at ca.1800Ma and 2500Ma). The peak ages of ca.1800Ma and 2500Ma are considered as typical age members of the North China Craton basement, suggesting the possible provenance derived from the North China Craton. Moreover, the other two age populations are closely consistent with the timing of magmatic events took place in the Erguna-Xing'an-Xilinhot blocks to the north of the Xar Moron suture zone. In comparison with variation trends of detrital components in sandstones which expose in the different regions (including, from southwest to northeast, the Hexigten Banner-Lixin area, the Ar Horqin Banner-Jarud Banner area and the Suolun-Moguqi area) with varying deposited time ranging from Mid-late Permian to Early Triassic, reveal that the ‘scissor-like’ closure process of the Paleo Asian Ocean, from west to east, and the terminated at least last to Early Triassic. In addition, the relative stable sources supplying of the Mid-late Permian to Early Triassic sandstones in the Suolun-Moguqi area, indicates that the Erguna-Xing'an block and Songliao-Xilinhot block has already collided along the Hegenshan-Heihe suture zone at the time before Mid-Permian deposits, should be as the previous report that of end of Early Carbonadoes. -
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