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UHPM eclogite of the Maksyutov complex (Southern Urals)

机译:Maksyutov建筑群(南乌拉尔)的UHPM榴辉岩

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摘要

This study reports the first find of a jadeite-bearing eclogite spatially associated with UHP ultramafic rocks of unit 1 of the Maksyutov complex (near the village of Karayanovo). Two phases of elcogitization were recognized based on mineralogical data, petrographic observations, and isotope geochronology. The first UHP metamorphic stage (533 +/- 4.6 Ma, P > 4.4 GPa, T > 700A degrees C) was defined by the assemblage jadeite + grossular-almandine + rutile +/- phengite. This assemblage was later transformed into omphacite + grossular-almandine + phengite + albite + clinozoisite + titanite at a retrograde phase of stage I (392-485 +/- 2-4 Ma, P > 3.1-3.4 GPa, T > 633-740A degrees C) with decreasing pressure and temperature. The second prograde phase (360 +/- 3 Ma, P > 1.1-2.2 GPa, T > 450-550A degrees C) of HP metamorphism was marked by the development of a chlorite rim (almandine-grossular-pyrope-almandine-grossular, diopside, clinozoisite) around the eclogite body. A comparison shows that the studied eclogite and ultramafic rocks followed a common P-T-t path. Jadiet-bearing eclogites and meta-ultramafic rocks represent UHPM fragments of the mantle and crust, which were tectonically emplaced in quartzite schists of unit 1.
机译:这项研究报告了在空间上与Maksyutov复合体1单元(卡拉扬诺沃村附近)的UHP超镁铁质岩石在空间上相关的含翡翠的榴辉岩的发现。根据矿物学数据,岩石学观测和同位素年代学,电凝作用分为两个阶段。 UHP的第一个变质阶段(533 +/- 4.6 Ma,P> 4.4 GPa,T> 700A摄氏度)是由组合翡翠+粒状金刚烷+金红石+/-锂铁矿定义的。在第一阶段的逆行阶段(392-485 +/- 2-4 Ma,P> 3.1-3.4 GPa,T> 633-740A),该组合物随后转变为绿辉石+硬脂金刚烷+扁桃石+钠长石+斜长石+钛铁矿摄氏度)。 HP变质的第二个前进阶段(360 +/- 3 Ma,P> 1.1-2.2 GPa,T> 450-550A摄氏度)以亚氯酸盐边缘(金刚烷-罗汉果-吡咯烷-金刚玉-罗汉果,透辉石体周围的透辉石,斜长石)。比较表明,研究的榴辉岩和超镁铁质岩石遵循相同的P-T-t路径。含Jadiet的榴辉岩和超超镁铁质岩石代表着地幔和地壳的UHPM碎片,这些碎片被构造地放置在1号单元的石英岩片岩中。

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  • 来源
    《Doklady Earth Sciences》 |2015年第1期|291-296|共6页
  • 作者单位

    Russian Acad Sci, Ural Branch, Ilmen State Reserve, Miass 456317, Russia;

    Russian Acad Sci, Zavaritskii Inst Geol & Geochem, Ural Branch, Ekaterinburg 620075, Russia;

    Russian Acad Sci, Zavaritskii Inst Geol & Geochem, Ural Branch, Ekaterinburg 620075, Russia;

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