摘要
在内蒙牙克石地区发育两种不同构造属性的岩石组合:一类为乌奴耳-头道桥蛇绿混杂岩,另一类为晚古生代弧属性侵入岩。乌奴耳-头道桥蛇绿混杂岩由辉长岩、辉长辉绿岩、辉绿玢岩(岩墙?)、变玄武岩和放射虫硅质岩组成;地球化学特征显示基性岩类属于拉斑玄武岩系列,具有相似的稀土和原始地幔标准化配分模式,与N-MORB的特征类似,不具有Nb-Ta负异常,Nb/Nb~*值平均>1;构造环境判别图显示该蛇绿混杂岩可能形成于扩张脊。晚古生代弧属性侵入岩出露于白井山、乌尔其汗,由中基性单元(辉长岩、辉长闪长岩和石英闪长岩)和酸性单元(花岗闪长岩和二长花岗岩)组成;地球化学特征显示中基性单元和酸性单元属于钙碱性岩系列,富集LREEs和LILEs,具有Nb-Ta负异常,高Sr、Sr/Y值,低HREEs和Y,Eu异常不明显;酸性单元显示埃达克质岩的地球化学特征。乌奴耳-头道桥蛇绿混杂岩可能形成于新元古代,与头道桥蓝片岩、吉峰蛇绿混杂岩、新林蛇绿岩构成一条重要的缝合带,暗示本区古洋盆的存在。晚古生代弧属性侵入岩中,辉长岩的结晶年龄为326±1.9Ma,花岗闪长岩的结晶年龄为323.7±1.9Ma;微量元素的组成特征显示,中基性单元和酸性单元的形成与早石炭世洋壳板片的俯冲作用有关,暗示兴安地块和松嫩地块之间洋盆的萎缩。
Two different types of rock assemblages exist in Yakeshi region, Inner Mongolia:one is Wunuer-Toudaoqiao ophiolitic mélange; the other is Late Paleozoic arc-type intrusion. The Wunuer-Toudaoqiao ophiolitic mélange comprises gabbro, gabbro-diabase, allgovite (dyke?), metabasalt and radiolarian siliceous rocks. The geochemical data show that the basic rocks from the Wunuer-Toudaoqiao ophiolitic mélange are tholeiitic series, and have consistent distributed patterns of REE and trace elements, similar to the features of N-MORB. They don't display negative Nb-Ta anomalies with ratios of Nb/Nb*〉1. Additionally, tectonic discrimination shows the Wunuer-Toudaoqiao ophiolitic mélange might have been formed in a spreading ridge. The Late Paleozoic arc-type intrusions outcrop in Baijingshan and Wuerqihan, and comprise a medium-basic unit (gabbro, gabbro diorite and quartz diorite) and an acidic unit (granodiorite and monzogranite). The geochemical data show that the medium-basic and acidic units are calc-alkali series, and enriched in LREEs and LILEs; they have negative Nb-Ta anomalies with high Sr concentrations and Sr/Y ratios; they show low HREE contents and Y concentrations without Eu anomalies. In addition, the acidic unit has geochemical features of adakitic rocks. The Wunuer-Toudaoqiao ophiolitic mélange might form in Neoproterozoic, which, together with Toudaoqiao blueschist, Jifeng ophiolite mélange and Xinlin ophiolite, consists of a vital suture zone, suggesting a Paleo-ocean once existed in Yakeshi region. The formation age of the gabbro and granodiorite from the Late Paleozoic arc intrusions is 326±1.9Ma and 323.7±1.9Ma, respectively. In terms of trace elements, we confirmed that the formation of the Late Paleozoic arc-type intrusions was related to Early Carboniferous oceanic slab subduction, suggesting the oceanic basin wither between Xing'an block and Songnen block.
作者
董金龙
白志达
徐德兵
罗志波
DONG JinLong;BAI ZhiDa;XU DeBing;LUO ZhiBo(MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China;School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China;Tianfin Geophysical Exploration Center, Tianjin 300170, China)
出处
《岩石学报》
SCIE
EI
CAS
CSCD
北大核心
2018年第6期1758-1774,共17页
Acta Petrologica Sinica
基金
中国地质调查局项目(1212011120657)资助
关键词
蛇绿混杂岩
扩张脊
弧属性
新元古代
晚古生代
牙克石地区
Ophiolitic m61ange
Spreading ridge
Arc affinity
Neoproterozoic
Late Paleozoic
Yakeshi region