The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching
Autor(a) principal: | |
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Data de Publicação: | 2019 |
Outros Autores: | , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.1016/j.lithos.2019.07.005 http://hdl.handle.net/11449/187904 |
Resumo: | Understanding the chemical etching effects in the crystalline structure of zircon grains is crucial to know their chemical composition, morphology and isotopic geochemistry. After chemical etching, the zircon grain can be classified as homogeneous heterogeneous, hybrid and anomalous depending on the surface fission-track density observed under an optical microscope. The complementary techniques such as optical microscopy, micro-Raman spectroscopy, scanning electron microscopy (imaging by cathodoluminescence and secondary electrons) and electron microprobe, were employed to characterize the zircon grain surfaces from Igneous, Metamorphic and Sedimentary rocks before and after chemical etching, except for Raman spectroscopy. Measurements of U-Pb age are concordant in areas on the grain surface with uniform fission-track density. The chemical and isotopic analyses show that the etching is capable of revealing the different layer imperfections of the zircon crystalline structure, which can be inherent in its crystallization or acquired during its geological history. Therefore, identification of crystallographic preserved areas on the zircon surface, which are associated with uniform fission-track density, helps to get highly concordant U-Pb ages. In general, the results showed that the U-Pb system depends significantly on the amorphization degree of the zircon crystalline structure, which in most cases can only be revealed by etching. |
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The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etchingCrystalline structureEtchingU-Pb systemZircon fission trackUnderstanding the chemical etching effects in the crystalline structure of zircon grains is crucial to know their chemical composition, morphology and isotopic geochemistry. After chemical etching, the zircon grain can be classified as homogeneous heterogeneous, hybrid and anomalous depending on the surface fission-track density observed under an optical microscope. The complementary techniques such as optical microscopy, micro-Raman spectroscopy, scanning electron microscopy (imaging by cathodoluminescence and secondary electrons) and electron microprobe, were employed to characterize the zircon grain surfaces from Igneous, Metamorphic and Sedimentary rocks before and after chemical etching, except for Raman spectroscopy. Measurements of U-Pb age are concordant in areas on the grain surface with uniform fission-track density. The chemical and isotopic analyses show that the etching is capable of revealing the different layer imperfections of the zircon crystalline structure, which can be inherent in its crystallization or acquired during its geological history. Therefore, identification of crystallographic preserved areas on the zircon surface, which are associated with uniform fission-track density, helps to get highly concordant U-Pb ages. In general, the results showed that the U-Pb system depends significantly on the amorphization degree of the zircon crystalline structure, which in most cases can only be revealed by etching.Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Department of Physics Paulista State University UNESPLaboratory of Geochronological Studies Geodynamics and Environment Institute of Geosciences University of BrasíliaDepartment of Physics Paulista State University UNESPFAPESP: 2011/14943-9FAPESP: 2014/15838-2Universidade Estadual Paulista (Unesp)University of BrasíliaResende, Rosana Silveira [UNESP]Tello Sáenz, Carlos Alberto [UNESP]Pereira, Luiz Augusto Stuani [UNESP]Dantas, Elton Luiz2019-10-06T15:50:52Z2019-10-06T15:50:52Z2019-12-15info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.1016/j.lithos.2019.07.005Lithos, v. 346-347.1872-61430024-4937http://hdl.handle.net/11449/18790410.1016/j.lithos.2019.07.0052-s2.0-85069718010Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengLithosinfo:eu-repo/semantics/openAccess2021-10-23T20:19:29Zoai:repositorio.unesp.br:11449/187904Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T20:08:01.992136Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching |
title |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching |
spellingShingle |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching Resende, Rosana Silveira [UNESP] Crystalline structure Etching U-Pb system Zircon fission track |
title_short |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching |
title_full |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching |
title_fullStr |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching |
title_full_unstemmed |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching |
title_sort |
The effect of chemical and physical imperfections in zircon grains in influencing the U-Pb age analyses: Insights from zircon fission track etching |
author |
Resende, Rosana Silveira [UNESP] |
author_facet |
Resende, Rosana Silveira [UNESP] Tello Sáenz, Carlos Alberto [UNESP] Pereira, Luiz Augusto Stuani [UNESP] Dantas, Elton Luiz |
author_role |
author |
author2 |
Tello Sáenz, Carlos Alberto [UNESP] Pereira, Luiz Augusto Stuani [UNESP] Dantas, Elton Luiz |
author2_role |
author author author |
dc.contributor.none.fl_str_mv |
Universidade Estadual Paulista (Unesp) University of Brasília |
dc.contributor.author.fl_str_mv |
Resende, Rosana Silveira [UNESP] Tello Sáenz, Carlos Alberto [UNESP] Pereira, Luiz Augusto Stuani [UNESP] Dantas, Elton Luiz |
dc.subject.por.fl_str_mv |
Crystalline structure Etching U-Pb system Zircon fission track |
topic |
Crystalline structure Etching U-Pb system Zircon fission track |
description |
Understanding the chemical etching effects in the crystalline structure of zircon grains is crucial to know their chemical composition, morphology and isotopic geochemistry. After chemical etching, the zircon grain can be classified as homogeneous heterogeneous, hybrid and anomalous depending on the surface fission-track density observed under an optical microscope. The complementary techniques such as optical microscopy, micro-Raman spectroscopy, scanning electron microscopy (imaging by cathodoluminescence and secondary electrons) and electron microprobe, were employed to characterize the zircon grain surfaces from Igneous, Metamorphic and Sedimentary rocks before and after chemical etching, except for Raman spectroscopy. Measurements of U-Pb age are concordant in areas on the grain surface with uniform fission-track density. The chemical and isotopic analyses show that the etching is capable of revealing the different layer imperfections of the zircon crystalline structure, which can be inherent in its crystallization or acquired during its geological history. Therefore, identification of crystallographic preserved areas on the zircon surface, which are associated with uniform fission-track density, helps to get highly concordant U-Pb ages. In general, the results showed that the U-Pb system depends significantly on the amorphization degree of the zircon crystalline structure, which in most cases can only be revealed by etching. |
publishDate |
2019 |
dc.date.none.fl_str_mv |
2019-10-06T15:50:52Z 2019-10-06T15:50:52Z 2019-12-15 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://dx.doi.org/10.1016/j.lithos.2019.07.005 Lithos, v. 346-347. 1872-6143 0024-4937 http://hdl.handle.net/11449/187904 10.1016/j.lithos.2019.07.005 2-s2.0-85069718010 |
url |
http://dx.doi.org/10.1016/j.lithos.2019.07.005 http://hdl.handle.net/11449/187904 |
identifier_str_mv |
Lithos, v. 346-347. 1872-6143 0024-4937 10.1016/j.lithos.2019.07.005 2-s2.0-85069718010 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Lithos |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
Scopus reponame:Repositório Institucional da UNESP instname:Universidade Estadual Paulista (UNESP) instacron:UNESP |
instname_str |
Universidade Estadual Paulista (UNESP) |
instacron_str |
UNESP |
institution |
UNESP |
reponame_str |
Repositório Institucional da UNESP |
collection |
Repositório Institucional da UNESP |
repository.name.fl_str_mv |
Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP) |
repository.mail.fl_str_mv |
|
_version_ |
1808129163448549376 |