{"title":"埃及东部沙漠Wadi Heimur地区的密西西比有孔矿物大理石","authors":"Abd-Elmohsen A. Ahmed","doi":"10.1016/0899-5362(87)90006-6","DOIUrl":null,"url":null,"abstract":"<div><p>A soft foraminiferal graphitic marble band of 3 m thickness overlying and grading into a grey laminated marble band up to 40 m in thickness interbanded with low grade eugeosynclinal metasediments and metavolcanics is exposed in the Wadi Heimur Area to the east of Lake Nasser. It has been considered previously as Pre-Cambrian (El Shazly <em>et al</em>. 1973, 1977 and Hunting 1967). The graphitic marble contains rare arenaceous Mississippian foraminifera comprising <em>Ammobaculites, Lituotubella</em> cl., <em>Palaeospiroplectammina</em> cf. <em>mellina, Trochammina</em> and <em>Endothyra</em>.</p></div>","PeriodicalId":100749,"journal":{"name":"Journal of African Earth Sciences (1983)","volume":"6 5","pages":"Pages 677-679"},"PeriodicalIF":0.0000,"publicationDate":"1987-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0899-5362(87)90006-6","citationCount":"1","resultStr":"{\"title\":\"Mississippian foraminiferal marble from Wadi Heimur Area, Eastern Desert, Egypt\",\"authors\":\"Abd-Elmohsen A. Ahmed\",\"doi\":\"10.1016/0899-5362(87)90006-6\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>A soft foraminiferal graphitic marble band of 3 m thickness overlying and grading into a grey laminated marble band up to 40 m in thickness interbanded with low grade eugeosynclinal metasediments and metavolcanics is exposed in the Wadi Heimur Area to the east of Lake Nasser. It has been considered previously as Pre-Cambrian (El Shazly <em>et al</em>. 1973, 1977 and Hunting 1967). The graphitic marble contains rare arenaceous Mississippian foraminifera comprising <em>Ammobaculites, Lituotubella</em> cl., <em>Palaeospiroplectammina</em> cf. <em>mellina, Trochammina</em> and <em>Endothyra</em>.</p></div>\",\"PeriodicalId\":100749,\"journal\":{\"name\":\"Journal of African Earth Sciences (1983)\",\"volume\":\"6 5\",\"pages\":\"Pages 677-679\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1987-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0899-5362(87)90006-6\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of African Earth Sciences (1983)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0899536287900066\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of African Earth Sciences (1983)","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0899536287900066","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
摘要
在纳赛尔湖以东的Wadi Heimur地区,暴露出一层厚度为3 m的软质有孔岩石墨大理岩带,其上覆为厚度达40 m的灰色层状大理岩带,并与低级的古地槽变质沉积物和变质火山相互交错。它以前被认为是前寒武纪(El Shazly et al. 1973,1977 and Hunting 1967)。石墨大理石含有稀有的砂质密西西比有孔虫,包括Ammobaculites, Lituotubella等。,古ospiroplectammina cf. mellina, Trochammina和Endothyra。
Mississippian foraminiferal marble from Wadi Heimur Area, Eastern Desert, Egypt
A soft foraminiferal graphitic marble band of 3 m thickness overlying and grading into a grey laminated marble band up to 40 m in thickness interbanded with low grade eugeosynclinal metasediments and metavolcanics is exposed in the Wadi Heimur Area to the east of Lake Nasser. It has been considered previously as Pre-Cambrian (El Shazly et al. 1973, 1977 and Hunting 1967). The graphitic marble contains rare arenaceous Mississippian foraminifera comprising Ammobaculites, Lituotubella cl., Palaeospiroplectammina cf. mellina, Trochammina and Endothyra.