Structure of the Padul-Nigueelas Basin (S Spain) from H/V Ratios of Ambient Noise: Application of the Method to Study Peat and Coarse Sediments
-This paper presents the results of the application of a technique of geophysical surveying based on resonance frequency of materials, in a small basin within the Internal Zones of the Betic Cordillera (southern Spain). The frequencies determined have enabled the main features of the basin's st...
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Veröffentlicht in: | Pure and applied geophysics 2002-09, Vol.159 (11-12), p.2733-2749 |
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creator | Delgado, J Alfaro, P Galindo-Zaldivar, J Jabaloy, A Lopez Garrido, AC Sanz de Galdeano, C |
description | -This paper presents the results of the application of a technique of geophysical surveying based on resonance frequency of materials, in a small basin within the Internal Zones of the Betic Cordillera (southern Spain). The frequencies determined have enabled the main features of the basin's structure to be delineated, clearly identifying its asymmetry due to variations in the position of the rigid basement in different sectors. The results show that this method does not guarantee a perfect identification of coarse sediments, unless these overlie substantial more rigid materials. On the other hand, the same method was very effective for studying very soft sediments (peat), and it was possible to establish a quantitative relationship for determining the thickness of these sediments based on their resonance frequency. This relationship was then used to map peat thickness in the basin. The results have been compared with gravity studies and mechanical drillings undertaken in the region. |
doi_str_mv | 10.1007/s00024-002-8756-1 |
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The frequencies determined have enabled the main features of the basin's structure to be delineated, clearly identifying its asymmetry due to variations in the position of the rigid basement in different sectors. The results show that this method does not guarantee a perfect identification of coarse sediments, unless these overlie substantial more rigid materials. On the other hand, the same method was very effective for studying very soft sediments (peat), and it was possible to establish a quantitative relationship for determining the thickness of these sediments based on their resonance frequency. This relationship was then used to map peat thickness in the basin. The results have been compared with gravity studies and mechanical drillings undertaken in the region.</description><identifier>ISSN: 0033-4553</identifier><identifier>EISSN: 1420-9136</identifier><identifier>DOI: 10.1007/s00024-002-8756-1</identifier><language>eng</language><subject>Asymmetry ; Basements ; Basins ; Borings ; Geophysics ; Gravitation ; Peat ; Sediments</subject><ispartof>Pure and applied geophysics, 2002-09, Vol.159 (11-12), p.2733-2749</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,781,785,27929,27930</link.rule.ids></links><search><creatorcontrib>Delgado, J</creatorcontrib><creatorcontrib>Alfaro, P</creatorcontrib><creatorcontrib>Galindo-Zaldivar, J</creatorcontrib><creatorcontrib>Jabaloy, A</creatorcontrib><creatorcontrib>Lopez Garrido, AC</creatorcontrib><creatorcontrib>Sanz de Galdeano, C</creatorcontrib><title>Structure of the Padul-Nigueelas Basin (S Spain) from H/V Ratios of Ambient Noise: Application of the Method to Study Peat and Coarse Sediments</title><title>Pure and applied geophysics</title><description>-This paper presents the results of the application of a technique of geophysical surveying based on resonance frequency of materials, in a small basin within the Internal Zones of the Betic Cordillera (southern Spain). The frequencies determined have enabled the main features of the basin's structure to be delineated, clearly identifying its asymmetry due to variations in the position of the rigid basement in different sectors. The results show that this method does not guarantee a perfect identification of coarse sediments, unless these overlie substantial more rigid materials. On the other hand, the same method was very effective for studying very soft sediments (peat), and it was possible to establish a quantitative relationship for determining the thickness of these sediments based on their resonance frequency. This relationship was then used to map peat thickness in the basin. The results have been compared with gravity studies and mechanical drillings undertaken in the region.</description><subject>Asymmetry</subject><subject>Basements</subject><subject>Basins</subject><subject>Borings</subject><subject>Geophysics</subject><subject>Gravitation</subject><subject>Peat</subject><subject>Sediments</subject><issn>0033-4553</issn><issn>1420-9136</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNqFjLFOwzAURS0EEqXwAWxvLIOp7Th2wlYqoEilVKRirV4dhxqlcYidga_gl2kFzCznDvfeQ8glZ9ecMT0OjDEh6R4006mi_IgMuBSM5jxRx2TAWJJQmabJKTkL4Z0xrnWaD8hXEbvexL6z4CuIWwtLLPuaLtxbb22NAW4xuAZGBRQtuuYKqs7vYDZ-hReMzofDbbLbONtEWHgX7A1M2rZ25tA2f9InG7e-hOihiH35CUuLEbApYeqxCxYKW7rdXhHOyUmFdbAXvzkkq_u71XRG588Pj9PJnGKWC6pygwZ1ydnGJCYTSleylDIvpVbCMlXtsdl3SgqJaAxWVqsMdSI5qpynyZCMfrRt5z96G-J654KxdY2N9X1Yc6V5ykWuxf9TxrlgSuk8-QYvpHWZ</recordid><startdate>20020901</startdate><enddate>20020901</enddate><creator>Delgado, J</creator><creator>Alfaro, P</creator><creator>Galindo-Zaldivar, J</creator><creator>Jabaloy, A</creator><creator>Lopez Garrido, AC</creator><creator>Sanz de Galdeano, C</creator><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20020901</creationdate><title>Structure of the Padul-Nigueelas Basin (S Spain) from H/V Ratios of Ambient Noise: Application of the Method to Study Peat and Coarse Sediments</title><author>Delgado, J ; Alfaro, P ; Galindo-Zaldivar, J ; Jabaloy, A ; Lopez Garrido, AC ; Sanz de Galdeano, C</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a892-69caca7d10bc3c8267f4d449d4762e06f2e0b0bc6424aaccafe768a7341a69153</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Asymmetry</topic><topic>Basements</topic><topic>Basins</topic><topic>Borings</topic><topic>Geophysics</topic><topic>Gravitation</topic><topic>Peat</topic><topic>Sediments</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Delgado, J</creatorcontrib><creatorcontrib>Alfaro, P</creatorcontrib><creatorcontrib>Galindo-Zaldivar, J</creatorcontrib><creatorcontrib>Jabaloy, A</creatorcontrib><creatorcontrib>Lopez Garrido, AC</creatorcontrib><creatorcontrib>Sanz de Galdeano, C</creatorcontrib><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Pure and applied geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Delgado, J</au><au>Alfaro, P</au><au>Galindo-Zaldivar, J</au><au>Jabaloy, A</au><au>Lopez Garrido, AC</au><au>Sanz de Galdeano, C</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Structure of the Padul-Nigueelas Basin (S Spain) from H/V Ratios of Ambient Noise: Application of the Method to Study Peat and Coarse Sediments</atitle><jtitle>Pure and applied geophysics</jtitle><date>2002-09-01</date><risdate>2002</risdate><volume>159</volume><issue>11-12</issue><spage>2733</spage><epage>2749</epage><pages>2733-2749</pages><issn>0033-4553</issn><eissn>1420-9136</eissn><abstract>-This paper presents the results of the application of a technique of geophysical surveying based on resonance frequency of materials, in a small basin within the Internal Zones of the Betic Cordillera (southern Spain). The frequencies determined have enabled the main features of the basin's structure to be delineated, clearly identifying its asymmetry due to variations in the position of the rigid basement in different sectors. The results show that this method does not guarantee a perfect identification of coarse sediments, unless these overlie substantial more rigid materials. On the other hand, the same method was very effective for studying very soft sediments (peat), and it was possible to establish a quantitative relationship for determining the thickness of these sediments based on their resonance frequency. This relationship was then used to map peat thickness in the basin. The results have been compared with gravity studies and mechanical drillings undertaken in the region.</abstract><doi>10.1007/s00024-002-8756-1</doi><tpages>17</tpages></addata></record> |
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subjects | Asymmetry Basements Basins Borings Geophysics Gravitation Peat Sediments |
title | Structure of the Padul-Nigueelas Basin (S Spain) from H/V Ratios of Ambient Noise: Application of the Method to Study Peat and Coarse Sediments |
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