Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks
Gypsum deposits are the currently exploited sulphate rocks with industrial purposes. In addition to the expensive drilling projects, geophysical techniques can be considered to estimate the economical potential of these deposits. An electrical resistivity tomography survey has been carried out in th...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2010 |
| País: | España |
| Institución: | Universidad de Barcelona |
| Repositorio: | Dipòsit Digital de la UB |
| OAI Identifier: | oai:diposit.ub.edu:2445/69559 |
| Acceso en línea: | https://hdl.handle.net/2445/69559 |
| Access Level: | acceso abierto |
| Palabra clave: | Roques sedimentàries Sedimentary rocks |
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Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocksGuinea Maysounave, AnderPlayà i Pous, ElisabetRivero Marginedas, LluísHimi, MahjoubRoques sedimentàriesSedimentary rocksGypsum deposits are the currently exploited sulphate rocks with industrial purposes. In addition to the expensive drilling projects, geophysical techniques can be considered to estimate the economical potential of these deposits. An electrical resistivity tomography survey has been carried out in the Pira gypsum formation (SE of the Catalan margin of the Tertiary Ebro Basin, Spain). Additionally, a continuous coring drill was performed in order to support the study. Electrical imaging has been successfully applied to identify the gypsum deposits interlayered in lutite units. Nevertheless, the gypsum-lutite boundaries are diffuse and uncertain in the tomographic lines. Comparison of the cores of the borehole and the electrical response shows a meaningful correlation between electrical resistivity and purity of gypsum. The electrical resistivity tomography profiles display a rather wide range of electrical resistivity value (from 20-1000 Ωm) for the investigated gypsum facies. The highest values are attributed to sulphate layers with >90% of gypsum mineral. Lutite units display higher values than expected due to the presence of evaporite minerals within them (>10 Ωm). Additionally, induced polarization measures have been performed in order to study the chargeability of gypsum deposits. It has been evidenced that impure gypsum rocks (with important presence of lutites within) are slightly chargeable. This property has allowed distinguishing between lutite levels and clay-rich gypsum rocks. Electrical resistivity tomography lines are useful in the prospection of gypsum deposits. However, electrical imaging prospection should be supported by an accurate petrological study of the deposits, in order to properly interpret the resistivity profiles.EAGE2010info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://hdl.handle.net/2445/69559Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésReproducció del document publicat a:Near Surface Geophysics, 2010, vol. 8, num. 3, p. 249-257(c) EAGE, 2010info:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/695592026-05-27T06:46:51Z |
| dc.title.none.fl_str_mv |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks |
| title |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks |
| spellingShingle |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks Guinea Maysounave, Ander Roques sedimentàries Sedimentary rocks |
| title_short |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks |
| title_full |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks |
| title_fullStr |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks |
| title_full_unstemmed |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks |
| title_sort |
Electrical resistivity tomography and induced polarisation techniques applied to the identifiaction of gypsum rocks |
| dc.creator.none.fl_str_mv |
Guinea Maysounave, Ander Playà i Pous, Elisabet Rivero Marginedas, Lluís Himi, Mahjoub |
| author |
Guinea Maysounave, Ander |
| author_facet |
Guinea Maysounave, Ander Playà i Pous, Elisabet Rivero Marginedas, Lluís Himi, Mahjoub |
| author_role |
author |
| author2 |
Playà i Pous, Elisabet Rivero Marginedas, Lluís Himi, Mahjoub |
| author2_role |
author author author |
| dc.subject.none.fl_str_mv |
Roques sedimentàries Sedimentary rocks |
| topic |
Roques sedimentàries Sedimentary rocks |
| description |
Gypsum deposits are the currently exploited sulphate rocks with industrial purposes. In addition to the expensive drilling projects, geophysical techniques can be considered to estimate the economical potential of these deposits. An electrical resistivity tomography survey has been carried out in the Pira gypsum formation (SE of the Catalan margin of the Tertiary Ebro Basin, Spain). Additionally, a continuous coring drill was performed in order to support the study. Electrical imaging has been successfully applied to identify the gypsum deposits interlayered in lutite units. Nevertheless, the gypsum-lutite boundaries are diffuse and uncertain in the tomographic lines. Comparison of the cores of the borehole and the electrical response shows a meaningful correlation between electrical resistivity and purity of gypsum. The electrical resistivity tomography profiles display a rather wide range of electrical resistivity value (from 20-1000 Ωm) for the investigated gypsum facies. The highest values are attributed to sulphate layers with >90% of gypsum mineral. Lutite units display higher values than expected due to the presence of evaporite minerals within them (>10 Ωm). Additionally, induced polarization measures have been performed in order to study the chargeability of gypsum deposits. It has been evidenced that impure gypsum rocks (with important presence of lutites within) are slightly chargeable. This property has allowed distinguishing between lutite levels and clay-rich gypsum rocks. Electrical resistivity tomography lines are useful in the prospection of gypsum deposits. However, electrical imaging prospection should be supported by an accurate petrological study of the deposits, in order to properly interpret the resistivity profiles. |
| publishDate |
2010 |
| dc.date.none.fl_str_mv |
2010 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
https://hdl.handle.net/2445/69559 |
| url |
https://hdl.handle.net/2445/69559 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
Reproducció del document publicat a: Near Surface Geophysics, 2010, vol. 8, num. 3, p. 249-257 |
| dc.rights.none.fl_str_mv |
(c) EAGE, 2010 info:eu-repo/semantics/openAccess |
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(c) EAGE, 2010 |
| eu_rights_str_mv |
openAccess |
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application/pdf |
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EAGE |
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EAGE |
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Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada) reponame:Dipòsit Digital de la UB instname:Universidad de Barcelona |
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Universidad de Barcelona |
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Dipòsit Digital de la UB |
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Dipòsit Digital de la UB |
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