Palaeocurrent directions as an indicator of Pindos foreland evolution (central and southern part), Western Greece

J. Vakalas, G. Ananiadis, J. Mpourlokas, D. Poulimenos, K. Getsos, G. Pantopoulos, P. Avramidis, A. Zelilidis, N. Kontopoulos
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引用次数: 3

Abstract

In order to estimate the palaeoflow direction of the submarine fans, deposited in the Internal Ionian subbasin of the Pindos Foreland, fifty-one positions along the sub-basin were selected and measurements of palaeocurrents indicators such as flute and groove marks were taken. In the studied area the main palaeoflow direction of turbidites was axial, from south to north in the southern part, and from north to south in the northern part. A minor westward palaeoflow direction is also present. These palaeoflow directions were influenced mainly by the regional tectonic activity, such as internal thrusting (Gavrovo Thrust) and differential activity of the Pindos Thrust which subdivided Pindos foreland into narrow linear sub-basins.
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古海流方向作为希腊西部品多斯前陆演化(中部和南部)的标志
为了估计滨多斯前陆内伊奥尼亚次盆地沉积的海底扇的古流动方向,选取了沿次盆地的51个位置,并测量了古水流的沟槽标志等指标。研究区浊积岩的主要古流动方向为轴向流,南部由南向北流,北部由北向南流。同时也存在少量西向古流动。这些古流动方向主要受区域构造活动的影响,如内部逆冲(加夫罗沃逆冲)和平多斯逆冲的差异活动,将平多斯前陆划分为狭窄的线状次盆地。
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