Mineralogy of The Beach Sands Along the Mediterranean Coast from Benghazi to Bin-Jawwad, NE Libya

O. R. Shaltami, A. El-Kammar, I. H. Arafa, F. F. Fares, يماتلاشلا ةماسأ
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Abstract

The present work aims to characterize the mineralogy of the beach sands along the Mediterranean Coast from Benghazi to Bin Jawwad, NE Libya. The microscopic and SEM examinations indicate an abundance of carbonates, quartz, feldspars, and evaporites. The detected heavy minerals are zircon, tourmaline, pistachite, hornblende, garnet, monazite, rutile, titanite, augite, biotite, kyanite, chromian spinel, magnetite, ilmenite, and goethite. Carbonate speciation suggests a difference in sediment age; the central and eastern sides consist of younger sediment, while older, reworked, and diagenetically transformed materials dominate in the western section. Three distinct groups of sediments can be recognized according to their mineral composition. The studied beach sands are mineralogically sub-mature sediments depending on the ZTR indices.
沿着地中海海岸从班加西到利比亚东北部的宾-乔瓦德的沙滩砂矿物学
目前的工作旨在表征海滩砂沿着地中海海岸从班加西到本Jawwad,利比亚东北部的矿物学。显微和扫描电镜检查显示碳酸盐、石英、长石和蒸发岩丰富。检测到的重矿物有锆石、电气石、开心石、角闪石、石榴石、独居石、金红石、钛矿、奥辉石、黑云母、蓝晶石、铬尖晶石、磁铁矿、钛铁矿和针铁矿。碳酸盐形态表明沉积年代不同;中部和东部由较年轻的沉积物组成,而西部以较老的、改造的和成岩转化的物质为主。根据沉积物的矿物组成,可以识别出三组不同的沉积物。从ZTR指标看,所研究的滩砂为矿物学上的亚成熟沉积物。
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