Morave Mt Oligocene-Middle Miocene succession of Albanian-Thessalian Basin

Bulletin of the Geological Society of Greece Pub Date : 2018-09-28 DOI:10.12681/BGSG.15837

P. Pashko

引用次数: 6

Abstract

The Morava Mountain Oligocene-Middle Miocene molasse deposits take part in the Albanian-Thessalian Basin, which developed NW-SE from eastern Albania to Thessaly in Greece, where it is called as Mesohellenic Basin. The 4.5 km thick basin infill is subdivided into three molasse cycles separated by two regional unconformities at the Eocene/Oligocene and Aquitanian/Burdigalian boundaries. The Morava Mountain Oligocene-Middle Miocene molase, ~ 3500 m thick, represents an exposed continuous, rich in fossil fauna succession. Six stratigraphic sections were studied and measured.

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Morave山渐新世-中中新世阿尔巴尼亚-色撒利亚盆地演替

莫拉瓦山渐新世-中中新世molasse矿床位于阿尔巴尼亚-色萨利盆地内，该盆地从阿尔巴尼亚东部向北西-东向希腊色萨利发育，被称为中希腊盆地。4.5 km厚的盆地充填被划分为3个molasse旋回，由始新世/渐新世和阿基坦期/Burdigalian边界的两个区域不整合面分隔。莫拉瓦山渐新世—中中新世molase，厚度约3500 m，为暴露连续，化石动物群演替丰富。研究测量了6个地层剖面。

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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Bulletin of the Geological Society of Greece

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