Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil)
Abstract The Guacuí and Batatal lineaments in the southern region of the state of Espírito Santo (southeastern Brazil) can be traced from satellite images for tens of kilometers. They are considered shear zones associated to the final tectonic stages of the Araçuaí-West Congo (A-WC) Orogen during th...
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| Format: | Article |
| Language: | English |
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Fundação Gorceix
2020-09-01
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| Series: | REM: International Engineering Journal |
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| Online Access: | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2448-167X2020000400499&tlng=en |
| _version_ | 1819258891143217152 |
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| author | Marcos Eduardo Hartwig Marilane Gonzaga de Melo César Augusto Moreira |
| author_facet | Marcos Eduardo Hartwig Marilane Gonzaga de Melo César Augusto Moreira |
| author_sort | Marcos Eduardo Hartwig |
| collection | DOAJ |
| description | Abstract The Guacuí and Batatal lineaments in the southern region of the state of Espírito Santo (southeastern Brazil) can be traced from satellite images for tens of kilometers. They are considered shear zones associated to the final tectonic stages of the Araçuaí-West Congo (A-WC) Orogen during the Ediacaran-Cambrian period. In order to understand their nature and tectonic implications for the development of the orogeny, we integrated geological and structural data based on fieldwork and detailed microstructural analysis. Data was collected along two profiles located at the central segments of both structures. The results demonstrated that the Guaçuí shear zone (GSZ) is a typical ductile transpressive shear zone with approximately 9 km width that shows numerous dextral kinematic indicators and records metamorphism of upper amphibolite facies. The GSZ shows different levels of intensity of dynamic deformation. The Batatal shear zone (BSZ) is a narrow brittle shear zone that shows essentially brittle microstructures (intercrystalline microfractures) revealing deformation at low-grade conditions (frictional regime). Based on their characteristics and the level of erosion of the rocks exposed in the region, we interpret that GSZ developed prior to BSZ. |
| first_indexed | 2024-12-23T19:01:19Z |
| format | Article |
| id | doaj.art-15c36711827e4842a2a3656721cacc65 |
| institution | Directory Open Access Journal |
| issn | 2448-167X |
| language | English |
| last_indexed | 2024-12-23T19:01:19Z |
| publishDate | 2020-09-01 |
| publisher | Fundação Gorceix |
| record_format | Article |
| series | REM: International Engineering Journal |
| spelling | doaj.art-15c36711827e4842a2a3656721cacc652022-12-21T17:34:42ZengFundação GorceixREM: International Engineering Journal2448-167X2020-09-0173449951210.1590/0370-44672020730043Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil)Marcos Eduardo Hartwighttps://orcid.org/0000-0002-2661-7506Marilane Gonzaga de Melohttps://orcid.org/0000-0003-3397-3258César Augusto Moreirahttps://orcid.org/0000-0002-9504-7025Abstract The Guacuí and Batatal lineaments in the southern region of the state of Espírito Santo (southeastern Brazil) can be traced from satellite images for tens of kilometers. They are considered shear zones associated to the final tectonic stages of the Araçuaí-West Congo (A-WC) Orogen during the Ediacaran-Cambrian period. In order to understand their nature and tectonic implications for the development of the orogeny, we integrated geological and structural data based on fieldwork and detailed microstructural analysis. Data was collected along two profiles located at the central segments of both structures. The results demonstrated that the Guaçuí shear zone (GSZ) is a typical ductile transpressive shear zone with approximately 9 km width that shows numerous dextral kinematic indicators and records metamorphism of upper amphibolite facies. The GSZ shows different levels of intensity of dynamic deformation. The Batatal shear zone (BSZ) is a narrow brittle shear zone that shows essentially brittle microstructures (intercrystalline microfractures) revealing deformation at low-grade conditions (frictional regime). Based on their characteristics and the level of erosion of the rocks exposed in the region, we interpret that GSZ developed prior to BSZ.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2448-167X2020000400499&tlng=enmylonitesmicrofracturesdeformationAraçuaí orogenshear zones |
| spellingShingle | Marcos Eduardo Hartwig Marilane Gonzaga de Melo César Augusto Moreira Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil) REM: International Engineering Journal mylonites microfractures deformation Araçuaí orogen shear zones |
| title | Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil) |
| title_full | Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil) |
| title_fullStr | Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil) |
| title_full_unstemmed | Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil) |
| title_short | Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil) |
| title_sort | structure and tectonic significance of high and low temperature deformation along the lateral escape related guacui and batatal shear zones southern aracuai orogen southeastern brazil |
| topic | mylonites microfractures deformation Araçuaí orogen shear zones |
| url | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2448-167X2020000400499&tlng=en |
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