阿尔泰南缘冲乎尔盆地康布铁堡组变质酸性火山岩年龄及岩石成因

摘要

The Chonghuer basin is one of the fault-bounded volcano-sedimentary basins on the southern margin of the Altay orogenic belt, where the Kangbutiebao Formation ( Fm. ) stratigraphic unithosted many economic deposits outcrops. LA-ICP-MS U-Pb zircon analyses from two meta-rhyolites and one meta-tuff of the Kangbutiebao Fm. in the Chonghuer Basin yield weighted mean 206Pb/238U ages of 385. 3 ± 1. 2Ma,398. 1 ± 1. 8Ma and 405. 6 ± 2. 2Ma, respectively, which can be interpreted as the eruption age of the Kangbutiebao silicic volcanic rocks in the Chonghuer Basin. The meta-rhyolites have similar geochemical features to meta-rhyolites in Kelang Basin and Maizi Basin, which are low-Ti rhyolite with obvious negative anomaly of Ti, P, Sr, Ba, Nb, Ta and Eu (δEu =0.25 ~ 0. 54) , obvious enrichment of Th, U, Pb, Zr, Hf and LREE. These features, together with the regional geological characteristics, indicate that these felsic volcanic rocks were generated by partial melting of lower crust on an active continental margin. These volcano-sedimentary basins are down-faulted Basin formed in compression tectonic environment of Early-Middle Devonian period.%冲乎尔盆地是阿尔泰南缘等间斜列的火山沉积盆地之一,盆地内出露有重要的康布铁堡组赋矿地层.本文对该组一个凝灰岩和两个变质流纹岩样品进行了LA-ICP-MS锆石U-Pb年龄测定,获得了385.3±1.2Ma、398.1±1.8Ma和405.6±2.2Ma的结果.变质流纹岩的岩石地球化学分析结果表明,与克朗和麦兹盆地内的酸性火山岩的特征相同,即变质流纹岩属钙碱性低Ti流纹岩；在原始地幔标准化图上显示出Ti、P、Sr、Ba明显负异常,Th、U、Pb的正异常,LREE相对HREE略富集的特征,并显示强的Eu负异常(δEu=0.25 ～0.54).结合其区域地质特征,认为本区变质酸性火山岩形成于活动大陆边缘环境,是下地壳发生了部分熔融后演化的产物.阿尔泰南缘的火山沉积盆地是早—中泥盆世时期在挤压环境中形成的断陷盆地.