Loutraki海湾地区海岸沉积物的研究

Α. Καραλη-Βουδουρη, Γ. Λειβαδιτησ, A. Μεττοσ
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引用次数: 0

摘要

对Loutraki湾沿岸沉积物的沉积学和矿物学特征进行了研究,包括对大量样品进行粒度分析、薄片研究和x射线检查。利用这些数据对沉积物的平均粒度、标准差σ、偏度SK和峰度KG等粒度参数进行了评价。基于平均粒度的沉积学参数研究表明,近海岸线为粗粒砂覆盖,而潮带为高能量环境。长岸漂移范围为Ν ~ s,近岸区砂的级配较为松散,前滩区砂的级配中等,后滩区砂的级配较好。它们的持续下降表明沉积物向南递进的趋势更好。后者与平均粒度相结合,表明动能从Ν降低到s。此外,还研究了滩岩的海拔和矿物组成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of the coastal sediments of the Loutraki gulf area
The study of the sedimentological and mineralogical characteristics of the coastal sediments in the Loutraki gulf, included analyses of a large number of samples, that is granulometry, thin section study and x-ray examination. From these data the granulometry paramètres were assessed such as mean grain size, standard deviation σ, skewness SK, and kurtosis KG of the sediments. The study of the sedimentological parameters based on the mean grain size the offshoreline is covered by coarse grain sand, whereas the tidal zone indicates a high energy environment. The longshoredrift is from Ν to S. Most of the sand is loosely graded in the nearschore area, medium graded in the foreshore area and well graded in the backshore area. Their constant declination indicates a trend for a better gradation of sediments southwards. The latter combined with the mean grain size indicate a reduction of kinetic energy from Ν to S. In addition, the beachrocks, were studied together with their, elevation and their mineral composition .
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