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Grain-size end-members and environmentally sensitive grain-size components: A comparative study in the mud shelf depocenters off southern Brazil

机译:颗粒大小的最终成员和对环境敏感的颗粒大小的组件:巴西南部附近泥架沉积中心的比较研究

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摘要

The current study aims to do a comparative analysis of the results obtained with two End-Member(EM)grain-size modeling techniques(AnalySize and BasEMMA)and the Environmental Sensitive Grain-Size(ESGS)modeling for sediment samples collected in the mudbelts of the southern Brazilian shelf.The methods were compared using grain-size data from the south Brazilian shelf,and the results are discussed here.It is the first time that the concept of ESGS,in its present form,is utilized outside China.The results show that despite its relative ease of use,the ESGS is not fully comparable to the EM analyses,and only two grain-size ESGS classes were recognized as analogous to EMs.The comparison of the AnalySize and BasEMMA procedures also revealed significant differences between the techniques.A comparative analysis between the two EM techniques revealed advantages in the BasEMMA,especially in the better correlation of the end-members with the original grain size distribution.The analysis of the geographical distribution of the EM abundances allowed point sources of sandy populations to be recognized as well as the contribution of the Rio de la Plata as a source of silty sediments to be inferred.

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  • 来源
    《国际泥沙研究(英文版)》 |2021年第2期|317-327|共11页
  • 作者单位

    Oceanographic Institute University of S(a)o Paulo Pra(c)a do Oceanográfico 191 S(a)o Paulo 05508-120 Brazil;

    Oceanographic Institute University of S(a)o Paulo Pra(c)a do Oceanográfico 191 S(a)o Paulo 05508-120 Brazil;

    Oceanographic Institute University of S(a)o Paulo Pra(c)a do Oceanográfico 191 S(a)o Paulo 05508-120 Brazil;

    Oceanographic Institute University of S(a)o Paulo Pra(c)a do Oceanográfico 191 S(a)o Paulo 05508-120 Brazil;

    Oceanographic Institute University of S(a)o Paulo Pra(c)a do Oceanográfico 191 S(a)o Paulo 05508-120 Brazil;

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  • 入库时间 2024-03-12 16:30:21
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