首页> 外文学位 >ARCHAEOLOGICAL GEOCHEMISTRY OF HIERAKONPOLIS IN THE NILE VALLEY, EGYPT (GEOLOGY, NEUTRON ACTIVATION ANALYSIS, SEDIMENTS, RARE EARTH ELEMENTS, TRACE).
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ARCHAEOLOGICAL GEOCHEMISTRY OF HIERAKONPOLIS IN THE NILE VALLEY, EGYPT (GEOLOGY, NEUTRON ACTIVATION ANALYSIS, SEDIMENTS, RARE EARTH ELEMENTS, TRACE).

机译:埃及尼勒河谷中的考古学地球化学(地质,中子活化分析,沉积物,稀土元素,痕量)。

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摘要

Hierakonpolis is an important archaelogical site linked to the first pharaohs of Egypt and as such provides important clues to understanding the development of the first nation state. At Hierakonpolis, the Predynastic archaeological artifacts are found in different types of sediments. It is difficult to differentiate these sedimentary units in the field because of their great geological similarities. Another source of difficulty arises in deciphering the environmental factors which affected the predynastic and early dynastic settlements in the Nile floodplain. It has been proposed that the trace element distributions in the various Nile sediments are different and highly related to how the Nile valley evolved with time. Instrumental Neutron Activation Analysis (INAA) was used to measure the trace elements in the Nile sediments and in several different size and mineral fractions taken from these sediments. The results of the distributions of trace elements in these sediments indicate that the various Nile silt units do have small differences in composition which can be used as a chemical fingerprint.; Trace element analysis of Predynastic pottery from Hierakonpolis that the pottery, straw tempered wares and finer untempered plum red wares, were made from particular Nile silt units and not from earlier geological deposits found in the immediate vicinity of the kilns. Mineralogical and chemical compositions of the major types of ceramic styles show that the variation among styles of pottery reflects kiln conditions and the treatment of pottery before the firing of the clay, rather than the firing temperature of the clay.
机译:希拉孔波利斯(Hierakonpolis)是与埃及第一个法老王有关的重要考古遗址,因此为了解第一个民族国家的发展提供了重要线索。在希拉孔波利斯,在不同类型的沉积物中发现了王朝前的考古文物。由于它们的巨大地质相似性,很难区分这些沉积单元。解读困难因素的另一个原因是,它会影响到尼罗河洪泛区的王朝前和王朝早期定居点。已经提出,各种尼罗河沉积物中的痕量元素分布是不同的,并且与尼罗河谷如何随时间演变密切相关。仪器中子活化分析(INAA)用于测量尼罗河沉积物中以及从这些沉积物中获取的几种不同大小和矿物组分中的微量元素。这些沉积物中痕量元素的分布结果表明,各种尼罗河泥沙单元的组成差异确实很小,可以用作化学指纹。希拉孔波利斯的王朝前陶器的微量元素分析表明,陶器,秸秆回火器皿和更精细的未回火的梅红色器皿是由特定的尼罗河泥沙单元制成的,而不是由窑炉附近早期的地质沉积物制成的。主要类型陶瓷样式的矿物学和化学组成表明,陶器样式​​之间的差异反映了窑烧成之前窑的条件和陶器的处理方式,而不是粘土的烧成温度。

著录项

  • 作者

    HAMROUSH, HANY AHMED.;

  • 作者单位

    University of Virginia.;

  • 授予单位 University of Virginia.;
  • 学科 Geochemistry.
  • 学位 Ph.D.
  • 年度 1985
  • 页码 355 p.
  • 总页数 355
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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