首页> 外文期刊>Journal of South American earth sciences >Characterization of phyllite weathering profiles developed under tropical climate on Quadrilátero Ferrífero region, MG, Brazil
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Characterization of phyllite weathering profiles developed under tropical climate on Quadrilátero Ferrífero region, MG, Brazil

机译:在巴西斯巴兰省QuadriláteroFerrífero区的热带气候下开发的植物岩石风化曲线的特征

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摘要

Low-grade metamorphic rocks show limitations in relation to the evaluation of weathering effects on macroscopic characteristics of the rock matrix due to their fine texture. In addition, the anisotropic character and high weathering impose difficulties in the preparation of samples for laboratory tests commonly used in the acquisition of physical and mechanical parameters for geotechnical purposes. This paper presents the results of a study carried out on the characterization of weathering effects on the morphology of typical profiles and on textural and mineralogical characteristics and physical and mechanical properties of weathering products of phyllites under tropical climate. The authors selected three road cut slopes and different geological materials according to their weathered state. Samples were collected for microscopic description on petrographic thin sections, and to obtain index and mechanical properties, through point load test (PLT). Detailed descriptions were performed in the field and in situ strength was estimated with a Schmidt hammer. The results show that the geological structures had a strong influence in the weathering profile, controlling the morphology of studied profiles. Weathering process was not uniform in rocks when they reached a more advanced degree of degradation. However, physical parameters associated with mineralogy were useful in predicting and differentiation the stages of phyllite weathering.
机译:低级变质岩表明,由于它们的细纹,有关岩石基质宏观特性的评价的局限性。此外,各向异性特征和高风化在制备用于获得岩土工程目的的物理和机械参数的实验室测试的样品中造成困难。本文介绍了对典型谱的形态的表征以及热带气候下近局部风化产品的病态和纹理和矿物学特性和物理和力学性能的研究结果。作者根据他们的风化状态选择了三条路切口和不同地质材料。通过点负荷试验(PLT)收集对岩体薄切片上的微观描述的微观描述的样品。在现场进行详细描述,并用施密锤估计原位强度。结果表明,地质结构对耐候性有着强烈影响,控制了研究曲线的形态。当岩石的岩石时,风化过程并不均匀,当它们达到更高的降解程度时。然而,与矿物学相关的物理参数可用于预测和分化Phyllite风化的阶段。

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