Citation: | LI Ping, CHEN Junlu, ZHANG Yue, et al. The Formation Age of Intrusions from Tudigou–Chigou Region in Southern Margin of Shangdan Subduction–Accretion Belt and Its Geological Significance[J]. Northwestern Geology, 2023, 56(2): 10-27. DOI: 10.12401/j.nwg.2022020 |
Located in the south margin of Shangdan sunduction–accretion belt, intrusive rocks in Shanyang–Zhashui region are mainly formed in two stages: the former is Neoproterozoic (885~621 Ma), and the latter is Middle–Late Triassic and Early Cretaceous (233~132 Ma) that was a result of Qinling orogenic event during Indosinian–Yanshan period. Zirons LA–ICP–MS U–Pb dating of intrusions in Tudigou–Chigou region show them formed between 144.4 Ma and 158.8 Ma, during Late Jurassic and Early Cretaceous. Geochemical study on these rocks reveals, they are enriched in large ion lithophile element (LILE) and depleted in high field strength elements (HFSE), with a high ratio of Sr/Y. Combined with the research on regional magmatic evolution, intrusions formed between Late Jurassic and Early Cretaceous in Tudigou and Chigou may be controlled by the movement of western Pacific and NE faults. And also, with the crustal delamination and the addition of fluid from subduction–accretion belt in post–collision and post–orogenic stages, intrusions from Shanyang– Zhashui region are formed by the melting of crust in Middle–south Qinling.
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严松涛,吴青松,代雪健,李虎,辛重阳,朱利东. 四川新龙地区中酸性侵入岩年代学、地球化学及对甘孜-理塘洋演化过程的制约. 地质通报. 2024(Z1): 401-415 .
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李康宁,汤庆艳,栾晓刚,王玉玺,邓小华,杨宗枫. 西秦岭三叠纪大河坝组砂岩构造背景与物质来源. 西北地质. 2024(03): 113-127+301 .
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刘新伟,薛玉山,寸小妮. 南秦岭龙头沟金矿床石英Rb-Sr同位素测年及其地质意义. 地质找矿论丛. 2024(04): 469-477 .
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葛战林,顾雪祥,章永梅,郑艳荣,刘明,郝迪,王元伟. 南秦岭柞水-山阳矿集区金盆梁金矿床载金硫化物矿物学特征及成矿指示. 西北地质. 2023(05): 278-293 .
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俞胜,贾轩,姚皓骞,徐磊,赵斌斌,贾新勇. 西秦岭白龙江地区志留系迭部组岩石地球化学特征及碎屑锆石原位U–Pb年代学研究. 西北地质. 2023(05): 245-261 .
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