Gravimetric inversion and three-dimensional geological modelling of the Piquiri Syenite Massif, southern Brazil

IF 2.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Victor Soares Cardoso , Maria de Fátima Bitencourt , Jairo Francisco Savian , Robson dos Santos Aquino , Cristiane Butori Rivera
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引用次数: 0

Abstract

The Pelotas Batholith corresponds to the eastern margin of the Dom Feliciano Belt in southernmost Brazil. It comprises multiple intrusions formed by successive tectonic-magmatic processes during the Brasiliano / Pan-African Cycle. One of these intrusive igneous bodies is the Piquiri Syenite Massif (PSM), recently described as a multi-intrusive body formed by three successive pulses, dated by LA-MC-ICP-MS (U-Pb in zircon), with the oldest pulse located at the margins and the youngest in the centre of the intrusion. Pulse 1 (609.3 ± 1.5 Ma) comprises fine- to medium-grained equigranular syenite to quartz syenite and alkali-feldspar quartz syenite, with colour index M′15–30. Pulse 2 (603.4 ± 3.9 Ma) comprises medium- to coarse-grained equigranular alkali-feldspar syenite and alkali-feldspar quartz syenite, with colour index M′ 5–15 and fragments of Pulse 1 varieties. Pulse 3 (588.8 ± 3.1 to 583.2 ± 1.8)comprises medium- to coarse-grained inequigranular quartz syenites, with colour index M′ 2–10, containing fragments of pulses 1 and 2 varieties. As defined by the AMS data, the PSM magnetic fabric is concordant with the magmatic fabric, parallel to the outer edges of the body, dipping towards the centre. However, the construction and emplacement of the body have been the subject of different interpretations. The main objective of this work is to relate the general morphology of the massif and the behaviour of the pulses within the massif with the processes of formation and ascent of the magmas that have built it. For this, terrestrial geophysical surveys were carried out to obtain gravimetric data, with which the Bouguer Anomaly map was generated. Modelling by gravimetric inversion was carried out in nine profiles using tools from the Oasis Montaj software, which was the basis for constructing a three-dimensional geological model using the Leapfrog Geo software. Associating the geological model with the magmatic and magnetic foliations, including the magnetic lineation, it was possible to determine a change in behaviour between the youngest and the two oldest pulses related to the ascension process. In addition, the body’s general shape, with the greatest depths located in the eastern region, allowed us to relate the rise of magma to a structure in the region.

巴西南部Piquiri正长岩体的重力反演和三维地质建模
Pelotas岩基对应于巴西最南端的Dom Feliciano带的东部边缘。它包括由巴西利亚诺/泛非旋回期间连续的构造-岩浆过程形成的多个侵入体。其中一个侵入性火成岩体是Piquiri正长岩体(PSM),最近被描述为一个由三个连续脉冲形成的多侵入体,通过LA-MC-ICP-MS(锆石中的U-Pb)测年,最古老的脉冲位于侵入体的边缘,最年轻的脉冲位于入侵体的中心。脉冲1(609.3±1.5 Ma)包括细到中等粒度的等粒正长岩到石英正长岩和碱性长石石英正长,颜色指数为M′15–30。脉冲2(603.4±3.9 Ma)包括中粗粒等粒碱性长石正长岩和碱性长石石英正长岩,颜色指数为M′5–15,脉冲1品种的碎片。脉冲3(588.8±3.1至583.2±1.8)包括中粒至粗粒不等粒石英正长岩,颜色指数为M′2–10,包含脉冲1和脉冲2变种的碎片。根据AMS数据的定义,PSM磁性组构与岩浆组构一致,平行于矿体外缘,向中心倾斜。然而,尸体的建造和安放一直是不同解释的主题。这项工作的主要目的是将地块的一般形态和地块内脉冲的行为与建造地块的岩浆的形成和上升过程联系起来。为此,进行了地面地球物理调查,以获得重力数据,并据此生成布格异常图。使用Oasis Montaj软件的工具对九个剖面进行了重力反演建模,该软件是使用Leapfrog Geo软件构建三维地质模型的基础。将地质模型与岩浆和磁叶理(包括磁线理)联系起来,就有可能确定与提升过程有关的最年轻和最古老的两个脉冲之间的行为变化。此外,该岩体的总体形状,最深处位于东部地区,使我们能够将岩浆的上升与该地区的结构联系起来。
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来源期刊
Journal of Geodynamics
Journal of Geodynamics 地学-地球化学与地球物理
CiteScore
4.60
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: The Journal of Geodynamics is an international and interdisciplinary forum for the publication of results and discussions of solid earth research in geodetic, geophysical, geological and geochemical geodynamics, with special emphasis on the large scale processes involved.
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