地质通报2023，Vol.42Issue(12)：2060-2083,24.DOI:10.12097/j.issn.1671-2552.2023.12.004
东昆仑昆中缝合带的活化:来自石炭纪花岗岩的证据
Activation of the Central Kunlun Suture Zone,East Kunlun:Evidence from Carboniferous granites
摘要
Abstract
In this publication,we identified Carboniferous intrusions for the first time in the Aksu River area,which has been relatively poorly explored in the western part of the East Kunlun.The Aksu acidic complex is located in the west section of the Central Kunlun fault zone.Zircon LA-ICP-MS dating results reveal that the granodiorite porphyry was crystallized at 361+2.4 Ma,the monzogranite at 357.5+2.8 Ma,and the granodiorite at 354+4.3 Ma,indicating that these rocks were intruded during Late Devonian to Early Carboniferous(close to the west of Central Kunlun Suture Zone)and this stage of the magmatic event has not previously been publicly reported.Analysis of major elements classifies these rocks as belonging to the high potassium calc-alkaline to calc-alkaline and peraluminous series.Trace and rare earth elements indicate that all rocks are enriched in large ion lithophile elements(such as Th,U,Rb,K),light rare earth elements and depleted in high field strength elements(such as Nb,P,Ti).These granites have high initial 87Sr/86Sr(0.70612～0.71009),low whole-rock εNd(t)values(-7.1～-5.1)and relative ancient TDM2 model ages ranging from 1.51 Ga to 1.69 Ga,which is comparable to the composition of enriched mantle or crust in the East Kunlun Orogen.Mineralogical and geochemical analyses indicate that the rocks are I-type granites,formed by remelting of crustal material,suggesting that the Central Kunlun Suture Zone underwent extensional setting during the Carboniferous.Combined with the regional geology and available geochronological data,we propose that this extensional event should be the result of the initial expansion of a back-arc basin caused by subduction of the Paleo-Tethys Ocean,which also places the time of initial subduction of the Paleo-Tethys Ocean in the Carboniferous rather than the Permian.关键词
花岗岩/地壳重熔/断裂活化/阿克苏河/东昆仑/早石炭世/地质调查工程Key words
granite/crustal remelting/fracture reactivation/Aksu River/East Kunlun/Early Carboniferous/geological survey engineering分类
天文与地球科学引用本文复制引用
董越,刘畅,曹伟伟,关力伟,段星星,刘珉..东昆仑昆中缝合带的活化:来自石炭纪花岗岩的证据[J].地质通报,2023,42(12):2060-2083,24.基金项目
中国地质调查局项目《新疆且末县阿克苏河一带(J45E015010、J45E016009、J45E016010)1∶5万区域地质矿产调查》(编号:DD2016007907)、中国核工业地质局地勘费项目《川藏地区雅安-林芝段铀多金属资源评价研究》(编号:地GT2201) （J45E015010、J45E016009、J45E016010）
