Magmatic episodes in the Holy Cross Mountains, Poland – a new contribution from multi-age zircon populations

E. Krzemińska, L. Krzemiński
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引用次数: 2

Abstract

This contribution reports on new U–Pb zircon age data from magmatic rocks from the Holy Cross Mountains (HCM) of Poland. The analyzed samples were taken from lamprophyre and diabase veins of Podkranów and Janowice-2 as well as from tuff horizon of Kielce Beds (Ludlow). Internal morphologies have been investigated by SEM-BSE and cathodoluminescence images and they have been used as a guide for the selection of genetically various type of grains, e.g. potential auto-, ante- and xenocrysts, that were analyzed by ion microprobe. The U–Pb age of the magmatic events at 414.2 ±6.6 Ma (Kielce tuff), 322 ±12 Ma (Podkranów, lamprophyre), and 300±10 Ma (Janowice-2, diabase) confirmed the time frame of known magmatic activity reported within the HCM, as determined by 40Ar/39Ar geochronology in previous studies. The zircon investigation revealed also multiple populations with record of an earlier pulse of magma system (antecrysts), as well as abundant xenocrysts.
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波兰圣十字山的岩浆事件——多年龄锆石种群的新贡献
本文报道了波兰圣十字山(HCM)岩浆岩中新的U-Pb锆石年龄数据。分析样品取自Podkranów和Janowice-2的煌斑岩和辉绿岩脉,以及Kielce床(Ludlow)的凝灰岩层。利用SEM-BSE和阴极发光图像研究了其内部形态,并用离子探针分析了潜在的自晶、前晶和异晶等不同基因类型的晶粒的选择。岩浆活动的U-Pb年龄分别为414.2±6.6 Ma (Kielce凝灰岩)、322±12 Ma (Podkranów煌斑岩)和300±10 Ma (Janowice-2辉绿岩),证实了HCM内已知岩浆活动的时间框架,即先前研究中40Ar/39Ar的地质年代学。锆石研究还发现了多个具有早期岩浆系统脉冲记录的种群(前结晶),以及丰富的异结晶。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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ZŁOTO W POTOKACH I PEGMATYCIE Z REJONU STRZELINA ROZPOZNANIE LOKALIZACJI WYROBISK PIASKÓW I ŻWIRÓW WZGLĘDEM GRANIC GZWP ORAZ CIEKÓW POWIERZCHNIOWYCH NA OBSZARZE WOJEWÓDZTWA ŚLĄSKIEGO INTERPRETACJA ZMIENNOŚCI TEMPERATURY WODY W ŹRÓDLE NA WSCHODNIM STOKU ZAMECZKÓW (TATRY ZACHODNIE) NA PODSTAWIE CIĄGŁYCH OBSERWACJI MONITORINGOWYCH I NUMERYCZNEGO MODELU TRANSPORTU CIEPŁA PARAMETRY MIGRACJI ZANIECZYSZCZEŃ W ODPADACH FLOTACYJNYCH NA PODSTAWIE TERENOWEGO EKSPERYMENTU ZNACZNIKOWEGO NA PRZYKŁADZIE OBIEKTU UNIESZKODLIWIANIA ODPADÓW WYDOBYWCZYCH „GILÓW” ZRÓŻNICOWANIE TŁA HYDROGEOCHEMICZNEGO WÓD PODZIEMNYCH EKSPLOATOWANYCH W ZLEWNI BIEBRZY
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