关于南帝汶河哲支姆地层的年龄问题

Natal'ya Nikulova, K. Kulikova, A. Sandula
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引用次数: 0

摘要

我们描述了南天曼 Zhezhimparma 隆起带 Dzhezhim 地层砾岩中的碧玉卵石。该砾石具有带状结构。中央部分由蜕变的火山玻璃组成,周围是鲕粒状和壳状结构的岩石,由赤铁矿色素微粒状六角形石英集合体组成。我们得出的结论是,碎屑物质的来源之一是铁锰酸盐(前铁锰酸盐)造山运动的岩石,从年龄上看,其最后碰撞阶段为晚文登期。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On the question of the age of the Dzhezhim formation of the South Timan
We have described jasper pebbles from gravelites of the Dzhezhim formation on the Zhezhimparma uplift in the Southern Timan. The chip has a zonal structure. The central part is composed of devitrified volcanic glass and is surrounded by the rocks with an oolitic and crustified structure, composed of hematite-pigmented microgranular hexagonal quartz aggregates. We made a conclusion that one of the sources of the detrital material was rocks of timanide (preuralide) orogen, which final collision stage was Late Vendian by the age.
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