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首页> 外文期刊>Rocznik Polskiego Towarzystwa Geologicznego >ADVANTAGES AND LIMITATIONS OF INTERPRETATIONS OF EXTERNAL MORPHOLOGY OF DETRITAL ZIRCON: CASE STUDY OF THE ROPIANKA AND MENILITE FORMATIONS (SKOLE NAPPE, POLISH FLYSCH CARPATHIANS)
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ADVANTAGES AND LIMITATIONS OF INTERPRETATIONS OF EXTERNAL MORPHOLOGY OF DETRITAL ZIRCON: CASE STUDY OF THE ROPIANKA AND MENILITE FORMATIONS (SKOLE NAPPE, POLISH FLYSCH CARPATHIANS)

机译：碎屑锆石外部形貌解释的优势与局限性：以罗皮安卡岩和红云母岩层为例（SKELL NAPPE，波兰Flysch喀尔巴阡岩）

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摘要

The zircon populations from the Campanian–Maastrichtian part of the Ropianka (Upper Cretaceous– Palaeocene) and Menilite (Oligocene–lower Miocene) formations in the northern part of the Skole Nappe in Poland were examined to evaluate interpretations of the external morphology of detrital zircon in provenance research. The advantage of the zircon typology method, supplemented with elongation measurements, is that it may be applied successfully to comparisons of euhedral zircon populations from sedimentary deposits of different ages and unknown provenance. The zircon typology method, along with elongation measurements of zircons, contributes valuable data that supplement conventional heavy-mineral analyses. It also permits the recognition of potential source areas and rock types for further comparative research.
机译：研究了波兰Skole Nappe北部的Ropianka（上白垩统-古新世）Campanian-Maastrichtian部分和渐新世（Meolite）（渐新世-下中新世）地层中的锆石种群，以评估对碎屑锆石外部形态的解释来源研究。锆石类型学方法的优点是可以进行延伸率测量，它可以成功地用于比较不同年龄和出处不明的沉积物中的真石锆石种群。锆石类型学方法与锆石的伸长率测量一起，为补充常规的重矿物分析提供了有价值的数据。它还可以识别潜在的震源区和岩石类型，以进行进一步的比较研究。

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