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Contribui?§?£o ao conhecimento da evolu?§?£o geol?3gica do Sistema Riacho do Pontal a?? PE, BA, PI

机译:对Riacho do Pontal系统的演化知识有所贡献吗? PE,BA,PI

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The Riacho do Pontal System (RPS) is just the central part of a long Neoproterozoic orogenic development placed at the northern periphery of the S?£o Francisco Craton (SFC), from northeast (Sergipano belt) to southwest (Rio Preto belt). The basement of the foreland (SFC) and the backland (a??Morro do Estreito-Icai?§araa??) is mostly formed by Archean rocks, with some insertions of supracrustal and orthogneisses of Tonian age (Cariris Velhos cycle?). RPS exhibits a remarkable tectonic-metamorphic zoning from north to the south the backland; the internal zone (supracrustal terrigenous assemblages); the central zone (ocean floor rock assemblages); the external zone (supracrustal terrigenous assemblages); and the cratonic domain (SFC), remarked by the presence of a wide (& 200 km) foreland thrust and fold belt (to the south), formed by the Neoproterozoic pelitic-carbonatic cratonic cover. The processes of deformation were intense, presenting vergence towards south and southwest, resulting in reclined and overturned folds, reverse and thrust faults, nappes, and specially the occurrences of some klippen over the basement of the northern part of the CSF. The regional metamorphism was undertaken under amphibolite conditions, with some local retrogression to the greenschists facies. This paper presents a series of new geochronological determinations (Rb-Sr, Sm- Nd and U-Pb methods) of practically all rock types of the basement, supracrustals, and of the associated syncollisional granites. It was possible to discriminate some Archean nuclei (2740 a?? 2624 Ma), as basement (backland), and two different set of Neoproterozoic volcano-sedimentary rock units associated with granites, the first one of Eotonian age (980 a?? 940 Ma) and the second one positioned in the Cryogenian-Ediacaran boundary (ca. 635 Ma). A preliminary essay of a??wilsoniana?? tectonic evolution is here introduced for this south-western portion of the Borborema Province (the regional branching system of orogens).
机译:Riacho do Pontal系统(RPS)只是一个新元古代造山带发展的中心部分,它位于S?o Francisco Craton(SFC)的北部外围,从东北(Sergipano带)到西南(Rio Preto带)。前陆(SFC)和后陆(a ?? Morro do Estreito-Icai?§araa??)的基底大部分由太古宙岩石形成,并伴有Tonian时代的上壳和正片麻岩的插入(Cariris Velhos循环?)。 RPS在偏远地区从北向南显示出明显的构造变质带。内部区域(陆壳上陆相组合);中心区域(海底岩石组合);外部区域(陆壳上陆相组合);克拉通域(SFC),其特征是存在由新元古代的古生界-碳质克拉通盖层形成的宽(> 200 km)前陆逆冲带和褶皱带(向南)。变形过程很激烈,向南和西南呈趋向性,导致倾斜和翻转褶皱,反向和逆冲断层,尿布,特别是在CSF北部基底上出现了一些速滑笔。区域变质作用是在角闪石条件下进行的,对绿片岩相有些局部退缩。本文介绍了一系列新的地质年代学测定方法(Rb-Sr,Sm-Nd和U-Pb方法),适用于几乎所有类型的地下室,表壳岩层和相关的斜滑花岗岩。可以区分一些太古代的核(2740 a ?? 2624 Ma),作为基底(偏远地区),以及与花岗岩相关的两组新元古代火山沉积岩单元,这是伊奥托纪的第一个时代(980 a ?? 940) Ma),第二个位于冰冻期-Ediacaran边界(约635 Ma)。威尔逊安娜的初步论文这里介绍了Borborema省西南部(造山带的区域分支系统)的构造演化。

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