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首页> 外文期刊>Sedimentary geology >Provenance of passive-margin and syn-collisional units: Implications for the geodynamic evolution of the Southern Brasilia Orogen, West Gondwana
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Provenance of passive-margin and syn-collisional units: Implications for the geodynamic evolution of the Southern Brasilia Orogen, West Gondwana

机译:被动保证金和同步单元的出处:对南·巴西岛奥根氏岛,西吉兰纳的地磁演变的影响

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摘要

Collisional orogens are one of the most conspicuous features of plate tectonics on Earth. They record the dynamics of continent-continent amalgamation, often confined to linear deformational belts. The Southern Brasilia Orogen is one of the most well-studied and complete orogens of West Gondwana. Newly obtained isotopic data, coupled with previously published analyses, expand the occurrence of metamorphosed passive margin sequences (maximum depositional age of similar to 900 Ma), with a main source in the Sao Francisco paleocontinent, to large sections of the orogen previously interpreted, by some investigators, as related to younger active margin deposits. This has implications for the location of the suture zone: as most of the upper and lower nappes are dominated by metamorphosed passive margin deposits, the suture is probably located at the base of the uppermost nappe, related to the active margin (Paranapanema paleocontinent). Zircon (U-Pb and Lu-Hf) and whole-rock (Sm-Nd and geochemistry) data obtained for syn-collisional meta-graywackes (similar to 650-630 Ma), that uncomformably overlie passive-margin-related successions, point to a bimodal provenance from both the passive (Sao Francisco paleocontinent) and active (Paranapanema paleocontinent) margins, depending on the structural level from which the samples were collected. Despite the conspicuous zircon age differences, the maximum depositional age is the same for samples from the upper and the lower nappes. Furthermore, the meta-graywackes from the lower and upper nappes are petrographically and geochemically similar. This suggests concomitant deposition in a common collisional setting. Two metamorphic ages were obtained by U-Pb monazite dating at similar to 633 and 606 Ma, indicating that protracted medium-grade metamorphic conditions affected the Southern Brasilia Orogen. (C) 2020 Elsevier B.V. All rights reserved.
机译:碰撞Origens是地球上板构造中最引人注目的特征之一。他们记录了大陆大陆融合的动态,通常限制在线性变形皮带。南巴拉西亚orgen是西吉纳最受欢迎和完善的奥戈葛之一。新获得的同位素数据,与先前公布的分析相结合,扩大了变质被动缘序列的发生(最大沉积年龄与900 mA类似),在Sao Francisco古色地区的主要来源,以前解释的orgen的大部分术语一些调查员,与年轻主动保证金存款有关。这对缝线区的位置有影响:由于大多数上下纳图由变质被动垫沉积物主导,缝合线可能位于与主动边缘(ParanaPanema古线地)有关的最高纳皮的基础。锆石(U-PB和LU-HF)和全摇滚(SM-ND和地球化学)用于同步元 - 灰度(类似于650-630 mA)的数据,可不规则地覆盖无源边缘相关的继承,点根据所收集样品的结构级别,从被动(Sao Francisco古色地区)和活性(ParanaPanema古色地区)边距的双峰来源。尽管锆石年龄差异显着,但最大沉积年龄与上部和下部Nappes的样品相同。此外,来自下部和上部Nappes的荟萃磨碎是岩化和地球织化学相似的。这表明在共同的碰撞环境中伴随着沉积。通过U-Pb Monazite进行的两个变质年龄类似于633和606 mA获得,表明延长的中级变质条件影响了南巴拉西亚orenogen。 (c)2020 Elsevier B.v.保留所有权利。

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