O. R. Shaltami, A. El-Kammar, I. H. Arafa, F. F. Fares, يماتلاشلا ةماسأ
{"title":"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","authors":"O. R. Shaltami, A. El-Kammar, I. H. Arafa, F. F. Fares, يماتلاشلا ةماسأ","doi":"10.59743/jmset.v2i2.110","DOIUrl":null,"url":null,"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.","PeriodicalId":106154,"journal":{"name":"مجلة علوم البحار والتقنيات البيئية","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2016-12-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Mineralogy of The Beach Sands Along the Mediterranean Coast from Benghazi to Bin-Jawwad, NE Libya\",\"authors\":\"O. R. Shaltami, A. El-Kammar, I. H. Arafa, F. F. Fares, يماتلاشلا ةماسأ\",\"doi\":\"10.59743/jmset.v2i2.110\",\"DOIUrl\":null,\"url\":null,\"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.\",\"PeriodicalId\":106154,\"journal\":{\"name\":\"مجلة علوم البحار والتقنيات البيئية\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2016-12-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"مجلة علوم البحار والتقنيات البيئية\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.59743/jmset.v2i2.110\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"مجلة علوم البحار والتقنيات البيئية","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.59743/jmset.v2i2.110","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Mineralogy of The Beach Sands Along the Mediterranean Coast from Benghazi to Bin-Jawwad, NE Libya
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.