首页> 外文期刊>Acta geologica Polonica >The Paleogene and early Neogene stratigraphy of the Beskid S?decki Range and Lubovnianska Vrchovina (Magura Nappe, Western Outer Carpathians)
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The Paleogene and early Neogene stratigraphy of the Beskid S?decki Range and Lubovnianska Vrchovina (Magura Nappe, Western Outer Carpathians)

机译:Beskid S?decki山脉和Lubovnianska Vrchovina(Magura Nappe,西部喀尔巴阡山脉)的古近纪和新近纪早期地层

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The lithostratigraphy and biostratigraphy of the Bystrica/Tylicz and Krynica facies zones of the Magura Nappe?have been studied in the Beskid Sadecki Range and Lubovnianska Vrchovina (Polish and Slovak parts of the Western?Outer Carpathians respectively). The new, Tylicz Zone is established, and the Szczawnica, Zarzecze,?Magura and Kremna formations are redefined and described. These formations, spanning over 35 myrs, represent?a synorogenic deep-water turbidites depositional system that dominated the southern part of the Magura Basin?after the collision of the Alcapa Mega Unit with the Czorsztyn/Oravic ridge. The calcareous nannoplankton zones?NP14–NP25 (Middle Eocene to Late Oligocene) and NN1–NN2 (Early Miocene) were recognized.
机译:Magura Nappe?的Bystrica / Tylicz和Krynica相带的岩相地层学和生物地层学已在Beskid Sadecki山脉和Lubovnianska Vrchovina(分别为西喀尔巴阡山脉的波兰和斯洛伐克部分)进行了研究。建立了新的Tylicz地带,并对Szczawnica,Zarzecze,Magura和Kremna地层进行了重新定义和描述。这些地层跨度超过35迈尔,代表了由Alcapa Mega Unit与Czorsztyn / Oravic山脊碰撞后形成的,在马古拉盆地南部占主导地位的协同增效深水浊度沉积系统。钙质的浮游生物区带为NP14-NP25(中始新世至晚渐新世)和NN1-NN2(早中新世)。

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