From magmatic arc to a post-accretionary setting: Late Palaeozoic granitoid plutons in the northwestern Trans-Altai Zone, Mongolia

IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
P. Hanžl, V. Janoušek, K. Hrdličková, D. Buriánek, O. Gerel, B. Altanbaatar, J. Hora, P. Čoupek
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引用次数: 1

Abstract

The Trans-Altai Zone in the southern tract of the Central Asian Oceanic Belt is composed of Early Palaeozoic oceanic crust preserved in Ordovician to Devonian ophiolite fragments and Devonian–Carboniferous igneous arcs. The Edren and Baaran subzones at the NW tip of the Trans-Altai Zone were intruded by Late Palaeozoic plutons that have been examined by the combined geochronological and geochemical study. Mississippian subduction-related plutons intruded Devonian and Carboniferous volcano-sedimentary sequences in two magmatic pulses. The older, Tournaisian plutons (dated at 352 ± 1 and 347 ± 4 Ma) occur in both subzones; the younger Visean/Serpukhovian ones (331 ± 1 Ma) are found only at the northern boundary of the Edren Subzone. All Mississippian rocks are high-K calc-alkaline and characterised by a strong enrichment of hydrous fluid mobile lithophile elements over conservative Nb, Ta and Ti relative to normal mid-ocean ridge basalts. Low 87 Sr/ 86 Sr i (~ 0.7035–0.7038) and highly positive ε iNd values (+ 6.6 to + 5.2) suggest a relatively juvenile parental magma source with a short mean crustal residence. This corresponds well with the age of scarce inherited zircons, none of which is older than 530 Ma. The Early Permian post-tectonic plutons intruded the shallow crust of the Baaran Subzone (Devonian–Carboniferous flysch and Early Carboniferous volcanic arc). The prominent concentric body of the Aaj Bogd Pluton is composed of monzodiorites to monzogabbros (284 ± 1 and 294 ± 3 Ma) in its centre, surrounded by granite with syenite (282 ± 1 Ma) in the main mass of the pluton. Whole-rock Sr–Nd isotopic ratios match those of Carboniferous magmatic rocks, while trace-element patterns point to an intra-plate origin influenced by a fertile asthenospheric mantle component. On the other hand, the slightly older (290 ± 1 Ma) quartz syenites to alkali feldspar granites in the Baaran Subzone have spurious arc-like geochemistry inherited from their arc-related crustal source(s). Regional distribution of the numerous oval-shaped Early Permian alkaline post-orogenic plutons, some with A 2 -type granite affinity, follows the major Permian strike-slip zones spanning from the Dulate Arc in the west to the Khan Bogd Pluton in the east. These late, transcurrent zones apparently played an important role in late-orogenic magma generation, ascent and emplacement.
从岩浆弧到后增生环境:蒙古跨阿尔泰带西北部晚古生代花岗岩类深成岩体
中亚海洋带南部地区的跨阿尔泰带由保存在奥陶纪-泥盆纪蛇绿岩碎片中的早古生代海洋地壳和泥盆纪-石炭纪火成弧组成。跨阿尔泰带西北端的Edren和Baaran亚带被晚古生代深成岩体侵入,这些深成岩体已通过地质年代和地球化学联合研究进行了检查。密西西比俯冲相关的深成岩体以两个岩浆脉冲侵入泥盆纪和石炭纪火山沉积序列。较老的图尔奈期深成岩体(日期分别为352±1和347±4 Ma)出现在这两个子带中;较年轻的维宪阶/谢尔普霍夫阶(331±1Ma)仅在Edren亚带的北部边界发现。所有密西西比岩石均为高钾钙碱性岩石,其特征是相对于正常中海脊玄武岩而言,含水流体流动亲石元素比保守的Nb、Ta和Ti富集。低87 Sr/86 Sr i(~0.7035–0.7038)和高正εiNd值(+6.6至+5.2)表明,母岩浆源相对年轻,平均地壳驻留时间短。这与稀少的继承锆石的年龄非常吻合,这些锆石的年龄都不超过530 Ma。早二叠世后构造深成岩体侵入了Baaran亚带的浅地壳(泥盆纪-石炭纪复理石和早石炭纪火山弧)。Aaj Bogd Pluton突出的同心体由中心的二长闪长岩至二长辉长岩(284±1和294±3 Ma)组成,被岩体主体中的正长岩(282±1 Ma)花岗岩包围。全岩Sr–Nd同位素比率与石炭纪岩浆岩的同位素比率相匹配,而微量元素模式表明板块内起源受到肥沃软流圈地幔成分的影响。另一方面,Baaran亚带中稍老(290±1 Ma)的石英正长岩至碱长花岗岩具有从其弧相关地壳源继承的假弧状地球化学。许多椭圆形早二叠世碱性后造山深成岩体的区域分布,其中一些具有A2型花岗岩亲和力,遵循从西部的杜拉特弧到东部的Khan Bogd Pluton的主要二叠纪走滑带。这些晚期的横贯带显然在造山晚期的岩浆生成、上升和侵位中发挥了重要作用。
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来源期刊
Journal of Geosciences
Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-MINERALOGY
CiteScore
2.30
自引率
7.10%
发文量
15
审稿时长
>12 weeks
期刊介绍: The Journal of Geosciences is an international peer-reviewed journal published by the Czech Geological Society with support from the Czech Geological Survey. It accepts high-quality original research or review papers dealing with all aspects of the nature and origin of igneous and metamorphic rocks. The Journal focuses, mainly but not exclusively, on: -Process-oriented regional studies of igneous and metamorphic complexes- Research in structural geology and tectonics- Igneous and metamorphic petrology- Mineral chemistry and mineralogy- Major- and trace-element geochemistry, isotope geochemistry- Dating igneous activity and metamorphic events- Experimental petrology and mineralogy- Theoretical models of igneous and metamorphic processes- Mineralizing processes and mineral deposits. All the papers are written in English, even though they may be accompanied by an additional Czech abstract. Each contribution is a subject to peer review by at least two independent reviewers, typically at least one from abroad. The Journal appears 2 to 4 times a year. Formally it is divided in annual volumes, each of them including 4 issues.
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