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首页> 外文期刊>International Geology Review >Igneous and metamorphic geochronologic evolution of granitoids in the central Eastern Segment, southern Sweden
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Igneous and metamorphic geochronologic evolution of granitoids in the central Eastern Segment, southern Sweden

机译:瑞典南部东部中部花岗岩的火成岩和变质年代学演化

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The Eastern Segment abutting the Transscandinavian Igneous Belt (TIB) mostly consists of rocks with overlapping igneous ages. In the Eastern Segment west of Lake Vättern, granitoids of clear TIB affinity exhibit strong deformational fabrics. This article presents U-Pb zircon ages from 21 samples spanning the border zone between these deformed TIB rocks in the east, and more thoroughly reworked rocks in the west. Magmatic ages fall in the range 1710-1660 million years, irrespective of the degree of deformation, confirming the overlapping crystallization ages between deformed TIB rocks and orthogneisses of the Eastern Segment. A common history is further supported by leucocratic rocks of similar ages. Prolonged orogenic (magmatic) activity is suggested by continued growth of zircon at 1.66-1.60 Ga. Six of the weakly gneissic rocks show zircons with cathodoluminescence-dark patches and embayments, possibly partly replacing metamict parts of older magmatic crystals, with 207Pb/206Pb ages dominantly between 1460 and 1400 million years, whereas three of the gneisses have zircon rims with calculated ages of 1440-1430 million years. Leucosome formation took place at 1443 ± 9 and 1437 ± 6 Ma. The minimum age of SE-NW folds was determined by an undeformed 1383 ± 4 million years crosscutting aplitic dike. Sveconorwegian zircon growth was not found in any of the samples from the studied area. To our knowledge, 1.46-1.40 Ga metamorphism affecting the U-Pb zircon system has not previously been reported this far northeast in the Eastern Segment. We suggest that the E-W- to SE-NW-trending deformation fabrics in our field area were produced during the Hallandian-Danopolonian orogeny and escaped later, penetrative Sveconorwegian reworking.View full textDownload full textKeywordsTransscandinavian Igneous Belt, Eastern Segment, Hallandian-Danopolonian orogeny, U-Pb zircon SIMS geochronology, FennoscandiaRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00206814.2010.543785
机译:与跨斯堪的纳维亚火成岩带(TIB)相邻的东段主要由具有不同火成时代的岩石组成。在Vättern湖以西的东段,具有TIB亲和力的花岗岩类具有很强的变形结构。本文介绍了21个样品中的U-Pb锆石年龄,这些样品横跨东部这些变形的TIB岩石之间的边界区域,而西部则经过更彻底的改造。不论变形程度如何,岩浆年龄都在1710至1660万年之间,这证实了变形的TIB岩石和东部段的正片麻岩之间的重叠结晶年龄。相似历史的白垩纪岩石进一步支持了共同的历史。锆石在1.66-1.60 Ga处的持续增长表明了延长的造山活动(岩浆活动)。六块弱片麻岩岩石中的锆石具有阴极发光-深色斑块和浮雕,可能部分替换了较旧岩浆晶体的准成矿部分, 207 Pb / 206 Pb的年龄主要位于1460至1400百万年之间,而其中三个片麻岩具有锆石轮缘,计算的年龄为1440-14.3亿年。白细胞的形成发生在1443±9和1437±6 Ma。 SE-NW褶皱的最小年龄由未变形的1383±400万年横切顶墙堤坝确定。在研究区域的任何样品中均未发现Sveconorwegian锆石的生长。据我们所知,影响U-Pb锆石系统的1.46-1.40 Ga变质作用迄今尚未在东北段的东北部报道。我们建议我们田间地区的EW-SE-NW趋势变形织物是在Hallandian-Danopolonian造山运动期间产生的,后来又逃脱了穿透性的Sveconorwegian返工。查看全文下载全文关键词Transscandinavian Igneous Belt,Eastern Segment,Hallandian-Danopolonian造山运动, U-Pb锆石SIMS年代学,Fennoscandia相关变量addthis_config = {ui_cobrand:“泰勒和弗朗西斯在线”,servicescompact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,更多”,发布编号: ra-4dff56cd6bb1830b“};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00206814.2010.543785

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