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首页> 外文期刊>International Geology Review >Differences between Southalpine and Austroalpine quartzphyllite complexes Eastern Alps: results from zircon chemical compositions and Pb/Pb dating
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Differences between Southalpine and Austroalpine quartzphyllite complexes Eastern Alps: results from zircon chemical compositions and Pb/Pb dating

机译:东阿尔卑斯山的南高山和奥山高山石英岩复合体之间的差异:锆石化学成分和Pb / Pb测年的结果

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摘要

We applied the zircon evaporation method and zircon typological and compositional studies to detrital-zircon populations of quartzphyllite complexes of the Eastern Alps, including the Southalpine (Vetriolo and Recoaro) and the Austroalpine (Goldeck, Gailtal, and Thurntaler) complexes. Combined zircon morphology and geochemical and geochronological analyses (single-zircon evaporation technique) provided significant constraints for the age of the studied protoliths. The morphological study points out that zircons from Austroalpine and Southalpine quartzphyllites show substantial differences in terms of shape, colour, size, type of inclusions, cracks, and turbidity. Electron microprobe analyses (Si, Zr, Hf, P: HREE) indicate homogeneous compositions, suggesting common source areas characterized by granitoid rocks, whereas typology indicates the existence of two distinct groups. Zircon ages from the quartzphyllites are rather different, those from Austroalpine samples being younger than Southalpine ones. Pb-Pb zircon ages define two principal evolutionary sequences. The Austroalpine complexes are characterized by an older evolution typical of subduction-related magmatism. This started by 598 Ma N-MORB-type, mainly involving depleted mantle sources, and finished with 379-341 Ma acid suites typical of a crustal source. Southalpine complexes zircon ages show an evolution characterized by tholeiitic and 473 Ma alkaline within-plate basalt-type suites in both pre- and post-Early Ordovician units. It involved intraplate mantle metasomatism and an enrichment trend along multicomponent sources. These magmatic evolution lines can be related to a plate-tectonic scenario that involved terrane accretion in a progressively mature Neoproterozoic to Ordovician active margin and a subsequent Palaeo-Tethys passive margin along the north Gondwanan periphery.View full textDownload full textKeywordszircon, quartzphyllite, Southalpine, Austroalpine, evaporation methodRelated 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/10.1080/00206814.2011.561985
机译:我们将锆石蒸发方法以及锆石的类型学和成分研究应用于东部阿尔卑斯山(包括南高山(Vetriolo和Recoaro)和奥山高山(Goldeck,Gailtal和Thurntaler))的碎屑锆石配合物的碎屑锆石种群。锆石形态学与地球化学和年代学分析(单锆石蒸发技术)相结合,为所研究的原生岩的年龄提供了重要的限制。形态学研究指出,来自奥山高山和南高山石英叶石的锆石在形状,颜色,大小,包裹体类型,裂缝和浊度方面显示出实质性差异。电子探针分析(Si,Zr,Hf,P:HREE)表明成分均一,表明以花岗岩类岩石为特征的共同源区,而类型学表明存在两个不同的族群。石英晶石的锆石年龄相差很大,来自奥山高山样品的锆石年龄比南高山样品的年轻。铅锆石锆石年龄定义了两个主要的演化序列。奥索高山复合体的特征是与俯冲有关的岩浆作用具有典型的较老的演化。它以598 Ma的N-MORB型开始,主要涉及耗尽的地幔源,最后以379-341 Ma的地壳源酸套件结束。南高山复合物锆石年龄显示出一种演化特征,即在奥陶纪早期和之后的单元中都具有孔雀石型和473 Ma碱性板内玄武岩型套件。它涉及板内地幔交代作用和沿多组分源的富集趋势。这些岩浆演化线可能与板块构造场景有关,该板块构造场景包括在新元古代至奥陶纪活动边缘逐渐成熟的新元古代和随后沿冈瓦纳北部外围的古特提斯被动边缘的地壳增生。查看全文下载全文关键字:锆石,石英岩,南阿尔卑斯山,高山阿尔卑斯山蒸发方法,相关变量var 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:“ ra-4dff56cd6bb1830b” };添加到候选列表链接永久链接http://dx.doi.org/10.1080/00206814.2011.561985

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