Facies Structure and Quantitative Parameters of the Pleistocene Sediments of the Fiji Sea

被引：0
作者：
Levitan, M. A. [1 ]
Antonova, T. A. [1 ]
Koltsova, A. V. [1 ]
机构：
[1] RAS, Vernadsky Inst Geochem & Analyt Chem, Kosygina St 19, Moscow 119991, Russia
来源：
GEOCHEMISTRY INTERNATIONAL | 2019年 / 57卷 / 11期
基金：
俄罗斯基础研究基金会;
关键词：
bottom sediments; sedimentary basins; South Fiji Basin; Lau Basin; Tonga Ridge; Eopleistocene; Neopleistocene; areas; masses of dry sediment; volumes; masses of sediments per time unit; carbonate sediments; volcanogenic turbidites;
D O I：
10.1134/S0016702919110053
中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
Lithological-facies zonality of Neo- and Eopleistocene sediments from the Fiji Sea is described for the first time. Processing of corresponding maps and isopachite schemes using A.B. Ronov's volumetric method gave us an opportunity to calculate the quantitative parameters of sedimentation for distinguished types of Pleistocene sediments. Carbonate sediments dominate over other groups of sediments. Carbonate planktonic sediments have been more intensively accumulated in the Neopleistocene than in the Eopleistocene. The highest volcanotectonic activity is typical of Eopleistocene.
引用
收藏
页码：1230 / 1235
页数：6
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