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U-Pb zircon age of the Krásné Loučky tuffite: the dating of Visean flysch in the Moravo-Silesian Paleozoic Basin (Rhenohercynian Zone, Czech Republic)

机译:KrásnéLoučky凝灰岩的U-Pb锆石年龄:摩拉沃-西里西亚古生代盆地(Rhenohercynian地带,捷克共和国)的Visean flysch年代

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摘要

The only pre vi ous U-Pb zir con date for the the Early Car bon if er ous flysch se quence of the Moravo-Silesian Pa leo zoic Ba sinwas pub lished in 1987 from tuffogenic ma te rial from Kobylí Quarry at Krásné Louèky near the town of Krnov (Silesia, CzechRe pub lic). The mea sured age of 319 Ma did not agree with its strati graphic po si tion, and was used as the ba sis for a hy poth e -sized block of Late Car bon if er ous paralic molasse in cor po rated dur ing a later tec tonic event. Dur ing a sur vey of the still-ac -tive quarry in 2010, volcaniclastic ho ri zons were iden ti fied and sam pled. Di rect cor re spon dence of the tuff units to thosesam pled in 1987 can not be proved but is likely. High pre ci sion chem i cal abra sion – ther mal ion iza tion mass spec trom e try(CA-TIMS) U-Pb dat ing of zir con from this new ma te rial has yielded an age of 340.05 ± 0.22 Ma, which cor re lates to the pre vi -ously in ferred strati graphic age of the lo cal ity and the cur rent cal i bra tion of the Early Car bon if er ous geo logic time scale. Thenewly es tab lished age cor re sponds to the Visean stage and dates the bound ary be tween the Horní Benešov and Moravicefor ma tions that can be cor re lated with other foredeep bas ins of the Culm in the Eu ro pean Variscides. A pop u la tion of de tri talCambro-Or do vi cian zir cons and a sin gle 2.0 Ga old zir con crys tal from the same volcaniclastic layer dated by la ser ab la tionin duc tively cou pled plasma mass spec trom e try (LA-ICPMS) are con sis tent with the known age of source ma te rial in theVariscan orogenic front.
机译:如果Moravo-Silesian Pa leoicic Ba sinwa的有序飞行序列于1987年由科比·夸里Kobylí采石场的凝灰岩材料出版,附近的KrásnéLouèky早在此之前,唯一的U-Pb锆石存在。克尔诺夫镇(Silesia,CzechRe pub lic)。测得的319 Ma年龄与它的分层图形位置不一致,并且如果以后再定级时含有大量的顺糖蜜,则可以用作大块后期碳糖的基础。 tec补品事件。在2010年仍活跃的采石场进行的一次调查中,确定并采样了火山碎屑岩带。凝灰岩装置与1987年的凝灰岩装置的直接对应性无法得到证明,但有可能。高精度化学磨损–该新材料的锆石的热离子质谱法(CA-TIMS)U-Pb还原产生的年龄为340.05±0.22 Ma,如果存在地理逻辑时间标度,则可以追溯到当地的最早地层时代和早期碳酸盐的当前年代。新近建立的年龄对应于Visean阶段,并确定了HorníBenešov和Moravice之间的界限,这些界限可以与欧洲Variscides中Culm的其他前瞻性基底相关。三次Cam-Or doviian锆石的爆破和一个2.0 Ga老锆石的凝结来自同一激光火山碎屑层,该层由激光熔蚀法测定,可有效地产生等离子质谱图( LA-ICPMS)与Varisscan造山带前缘的已知物质年龄一致。

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