庞博宸,李秋根,陈隽璐,刘树文,王宗起,陈衍景,肖兵.东天山大南湖-头苏泉岛弧带古生代侵入岩浆活动期次及基底性质[J].西北地质,2020,(2):1-26 PANG Bochen,LI Qiugen,CHEN Junlu,LIU Shuwen,WANG Zongqi,CHEN Yanjing,XIAO Bing.Paleozoic Intrusive Magmatic Activity and Basement Properties of the Dananhu-Tousuquan Island Arc in the Eastern Tianshan Mountains[J].Northwestern Geology,2020,(2):1-26
东天山大南湖-头苏泉岛弧带古生代侵入岩浆活动期次及基底性质
Paleozoic Intrusive Magmatic Activity and Basement Properties of the Dananhu-Tousuquan Island Arc in the Eastern Tianshan Mountains
投稿时间:2020-02-25  修订日期:2020-04-03
DOI:10.19751/j.cnki.61-1149/p.2020.02.001
中文关键词:  地壳演化;锆石U-Pb定年;锆石Hf同位素;大南湖-头苏泉岛弧带;东天山
英文关键词:crustal evolution;zircon U-Pb dating;zircon Hf isotopes;Dananhu-Tousuquan island arc;eastern Tianshan Mountains
基金项目:国家重点基础研究发展计划(“九七三”计划)“新疆北部古弧盆体系成矿机理”项目(2014CB440801),中国地质调查局“准噶尔古生代增生造山的岩浆作用与成矿”项目(12120113041000),中国地质调查局“塔里木前寒武纪铁块成因类型及层控规律研究”项目(1212011140056)
作者单位E-mail
庞博宸 造山带与地壳演化教育部重点实验室, 北京大学球与空间科学学院, 北京 100871  
李秋根 造山带与地壳演化教育部重点实验室, 北京大学球与空间科学学院, 北京 100871 qgli@pku.edu.cn 
陈隽璐 中国地质调查局 西安地质调查中心, 陕西 西安 710054  
刘树文 造山带与地壳演化教育部重点实验室, 北京大学球与空间科学学院, 北京 100871  
王宗起 中国地质科学院矿产资源研究所, 北京 100037  
陈衍景 造山带与地壳演化教育部重点实验室, 北京大学球与空间科学学院, 北京 100871  
肖兵 中国科学院广州地球化学研究所, 广东 广州 510640  
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中文摘要:
      锆石U-Pb定年结果显示:东天山大南湖-头苏泉岛弧带中酸性侵入岩形成时代为古生代,处于465~265 Ma,可划分为4个期次。分别为:中奥陶世-晚志留世465~413 Ma、中-晚泥盆世391~377 Ma、石炭纪327~308 Ma,以及早-中二叠世284~269 Ma。锆石Hf同位素分析显示,锆石εHft)值为6.81~15.73,Hf同位素二阶段模式年龄为839~355 Ma,主要集中在598~429 Ma;465~413 Ma的侵入岩分布在卡拉塔格和大南湖,其εHft)值为11.34~15.20,相应的Hf同位素二阶段模式年龄为633~467 Ma;391~377 Ma的侵入岩分布于卡拉塔格,其εHft)值为6.81~13.32,相应的Hf同位素二阶段模式年龄为839~497 Ma;327~308 Ma的侵入岩分布在黄山西以及沁城南,其εHft)值为11.36~15.73,相应的Hf同位素二阶段模式年龄为575~429 Ma;284~269 Ma的侵入岩分布在土屋西和推克曼塔什,其εHft)值为8.94~14.51,相应的Hf同位素二阶段模式年龄是671~355 Ma。再结合前人的研究成果揭示,在大南湖-头苏泉岛弧带底部可能存在老的地壳基底,并对这些岩浆活动有所贡献;该区古生代期间存在大约465 Ma早奥陶世以及330 Ma左右中石炭世2期地壳增生事件,并存在晚奥陶世-晚志留世、中-晚泥盆世和早-中二叠世三期地壳再造事件。
英文摘要:
      Zircon U-Pb dating results show that the emplacement ages of intermediate-acid intrusive rocks in the Dananhu-Tousuquan island arc of the eastern Tianshan Mountains is between 465-265 Ma in the Paleozoic era. It can be divided into 4 periods:Middle Ordovician to Late Silurian (465-413 Ma), Middle Devonian (391-377 Ma), Carboniferous (327-308 Ma), and Early-Middle Permian (284-269 Ma). Zircon Hf isotope analysis shows that εHf (t) values range from 6.81 to 15.73 with the two-stage Hf model ages 839 Ma-355 Ma, mainly at 598 Ma-429 Ma. The intrusive rocks aged 465-413 Ma are distributed in Kalatage and Dananhu, with the εHf (t) values ranging from 11.34 to 15.20, and the two-stage Hf model ages ranging from 633 Ma to 467 Ma. The 391-377 Ma intrusive rocks occurred in the Karatag, with the εHf (t) value ranging from 6.81 to 13.32, and two-stage Hf model ages ranging from 839 Ma to 497 Ma. The intrusive rocks dated 327-308 Ma are exposed in the west of Huangshan and south of Qincheng, with the εHf (t) value ranging from 11.36 to 15.73, and the two-stage Hf model ages ranging from 575 Ma to 429 Ma. The intrusive rocks with ages of 284-269 Ma are distributed in the west of Tuwu and Tuikemantashi, with the εHf (t) value ranging from 8.94 to 14.51, and the two-stage Hf model ages ranging from 671 Ma to 355 Ma.Combined with previous studies, this paper guesses that the old crustal basements beneath the Dananhu-Tou Suquan island arc contribute a lot to the paleozoic magmatic activities. In Palaeozoic era there were significant crustal accretion events near the Early Ordovician 465 Ma and the Middle Carboniferous 330 Ma in the arc, whereas in Late Ordovician-Late Silurian, Middle-Late Devonian and Early-Middle Permian crustal-reworking events occurred.
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