In situ white mica Rb/Sr geochronology of the Leszczyniec metaigneous complex, West Sudetes: evidence of upper plate deformation at the onset of Variscan collision

IF 1.8 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
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Abstract

The Karkonosze-Izera Massif in the West Sudetes preserves evidence of subduction of the Saxothuringian Ocean beneath the Teplá-Barrandian Domain. Within the massif, the Leszczyniec metaigneous complex (LMC) is identified as the upper allochthon. It exhibits a unique structural history in comparison to the underlying allochthons, suggesting that the LMC records a distinctive tectonic history. To investigate the timing of this history, two orthogneisses were studied from a single outcrop of the LMC for in situ white mica Rb/Sr geochronology. The outcrop bears a southeast-dipping foliation (S1) and a north/northeast plunging stretching lineation (L1), defined by white mica and quartz. Quartz recrystallization textures, white mica chemistry (celadonite content of 0.23–0.47), preservation of igneous plagioclase phenocrysts, and the metamorphic mineral assemblage, all indicate maximum epidote–amphibolite facies conditions. Single-spot Rb/Sr dates were calculated from white mica using initial 87Sr/86Sr values obtained by titanite and epidote. Results are similar for both rocks, providing weighted averages of 352.4 ± 4.1 Ma (MSWD: 0.6; n: 24) and 349.3 ± 2.5 Ma (MSWD: 0.4; n: 31). The rocks are interpreted to have the same structural and metamorphic history; thus, a pooled weighted average of 350.1 ± 5.3 Ma (2σ) is reported as the timing of white mica (re)crystallization during S1 and L1 development in epidote–amphibolite facies conditions. This event is bracketed by the timing of blueschist-facies metamorphism for the subjacent middle (c. 364 Ma) and lower (c. 345–341 Ma) allochthons, associated with an east/southeast-plunging L1. Considering the different structural and metamorphic histories of the LMC compared to the subjacent allochthons, it is likely that the complex was extracted from the Teplá-Barrandian upper plate due to subduction erosion prior to collective exhumation and stacking of the Karkonosze-Izera Massif.

Graphical abstract

Abstract Image

西苏台德地区 Leszczyniec 元成岩复合体的原位白云母 Rb/Sr 地球年代学:瓦里斯坎碰撞开始时上板块变形的证据
摘要 西苏台德地区的卡尔科诺斯泽-伊泽拉山丘(Karkonosze-Izera Massif)保留了泰普拉-巴兰迪岩域下萨克森图林洋俯冲的证据。在该地块内,莱什奇涅克火成岩复合体(Leszczyniec metaigneous complex,LMC)被确定为上全新统。与下面的各层岩相相比,它表现出独特的构造历史,这表明 LMC 记录了独特的构造历史。为了研究这段历史的时间,对 LMC 的一个露头的两块正长片麻岩进行了原位白云母 Rb/Sr 地质年代研究。该露头具有东南倾斜褶皱(S1)和北/东北俯冲拉伸线纹(L1),由白云母和石英界定。石英再结晶纹理、白云母化学成分(青云母含量为 0.23-0.47)、火成岩斜长岩表晶的保存以及变质矿物组合都表明了最大的表斜辉长岩面条件。利用榍石和闪长岩获得的 87Sr/86Sr 初始值计算了白云母的单点 Rb/Sr 日期。两种岩石的结果相似,加权平均值分别为 352.4 ± 4.1 Ma(MSWD:0.6;n:24)和 349.3 ± 2.5 Ma(MSWD:0.4;n:31)。这些岩石被解释为具有相同的构造和变质历史;因此,报告的加权平均值为 350.1 ± 5.3 Ma (2σ),这是在表闪长岩面条件下 S1 和 L1 发育期间白云母(再)结晶的时间。这一事件与次邻近的中统(约 364 Ma)和下统(约 345-341 Ma)蓝晶岩成因变质作用的时间相括弧,与向东/向东南倾斜的 L1 有关。考虑到LMC的构造和变质历史不同于邻近的各地层,该复合体很可能是在Karkonosze-Izera地块集体掘起和堆积之前,由于俯冲侵蚀而从Teplá-Barrandian上板块中提取出来的。 图表摘要
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来源期刊
International Journal of Earth Sciences
International Journal of Earth Sciences 地学-地球科学综合
CiteScore
4.60
自引率
4.30%
发文量
120
审稿时长
4-8 weeks
期刊介绍: The International Journal of Earth Sciences publishes process-oriented original and review papers on the history of the earth, including - Dynamics of the lithosphere - Tectonics and volcanology - Sedimentology - Evolution of life - Marine and continental ecosystems - Global dynamics of physicochemical cycles - Mineral deposits and hydrocarbons - Surface processes.
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