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Sediment geochemistry and tectonic setting: Application of discrimination diagrams to early stages of intracontinental rift evolution, with examples from the Okavango and Southern Tanganyika rift basins

机译:沉积物地球化学和构造环境:判别图在陆内裂谷演化的早期阶段中的应用,以奥卡万戈和坦Tang尼喀南部裂谷盆地为例

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摘要

In this article, we have applied discriminant diagrams and bivariate plots for tectonic setting to Quaternary sediments from the East African Rift System (EARS). Sediment samples used in this study represent two different phases in early stage intracontinental rift evolution: the alluvial fan of the nascent Okavango system and a lacustrine basin within the relatively more mature Tanganyika system. The diagrams for tectonic setting for major elements place the majority of these EARS sediments within the passive margin (PM) setting. Passive margin sandstones are generally enriched in SiO_2 and depleted in Na_2O, CaO and TiO_2 reflecting their highly recycled nature. Based on major element discriminant diagrams, we propose two new fields for early stage intracontinental rift evolution (alluvial fan and lacustrine basin), within the previously defined passive margin field. The rare earth element (REE) patterns from both Okavango and Tanganyika sediments exhibit patterns similar to PAAS, with ash layers from the Rungwe volcanics in the Tanganyika samples exhibiting an enrichment in REE relative to the bulk sediment.
机译:在本文中,我们将判别图和二元图应用于构造背景,以研究来自东非裂谷系统(EARS)的第四纪沉积物。本研究中使用的沉积物样品代表了早期洲际裂谷演化的两个不同阶段:新生的Okavango系统的冲积扇和相对较成熟的Tanganyika系统中的湖盆。主要元素的构造环境图将这些EARS沉积物的大部分置于被动边缘(PM)环境内。被动边缘砂岩通常富含SiO_2,而贫化的Na_2O,CaO和TiO_2反映了它们的高度循环利用性。基于主要元素判别图,我们在先前定义的被动边缘场内,提出了两个新的早期大陆内部裂谷演化场(冲积扇和湖盆)。来自Okavango和Tanganyika沉积物的稀土元素(REE)模式表现出与PAAS相似的模式,Tanganyika样品中Rungwe火山的灰分层相对于整体沉积物表现出REE富集。

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