Loading…
The electrical conductivity of gabbro at high temperature and high pressure
The electric conductivity of gabbro has been measured at 1.0-2.0 GPa and 320-700°C, and the conduction mechanism has been analyzed in terms of the impedance spectra. Experimental results indicated that the electric conductivity depends on the frequency of alternative current. Impedance arcs represen...
Saved in:
Published in: | Acta geochimica 2002-07, Vol.21 (3), p.252-257 |
---|---|
Main Authors: | , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-a2567-20809639e1da759f5f48826819519a6bd15aba3f9653f47e27007009cbbe5d863 |
---|---|
cites | cdi_FETCH-LOGICAL-a2567-20809639e1da759f5f48826819519a6bd15aba3f9653f47e27007009cbbe5d863 |
container_end_page | 257 |
container_issue | 3 |
container_start_page | 252 |
container_title | Acta geochimica |
container_volume | 21 |
creator | Doujun, Wang Heping, Li Li, Yi Weigang, Zhang Congqiang, Liu Gengli, Suo Dongye, Ding |
description | The electric conductivity of gabbro has been measured at 1.0-2.0 GPa and 320-700°C, and the conduction mechanism has been analyzed in terms of the impedance spectra. Experimental results indicated that the electric conductivity depends on the frequency of alternative current. Impedance arcs representing the conduction mechanism of grain interiors are displayed in the complex impedance plane, and the mechanism is dominated at high pressure. These arcs occur over the range of 10^sup 2^ -k × 10^sup 5^ Hz (k is the positive integer from 1 to 9). On the basis of our results and previous work, it is concluded that gabbro cannot form any high conductivity layer (HCL) in the middle-lower crust.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1007/BF02831090 |
format | article |
fullrecord | <record><control><sourceid>wanfang_jour_proqu</sourceid><recordid>TN_cdi_wanfang_journals_zgdqhx_e200203007</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><wanfj_id>zgdqhx_e200203007</wanfj_id><sourcerecordid>zgdqhx_e200203007</sourcerecordid><originalsourceid>FETCH-LOGICAL-a2567-20809639e1da759f5f48826819519a6bd15aba3f9653f47e27007009cbbe5d863</originalsourceid><addsrcrecordid>eNp1kM1OwzAQhC0EEqVw4QksOIEUWNvx3xEqCohKXMo5chI7SdUmqZ0A5elJFaSeOO1q9O2OZhC6JHBHAOT94xyoYgQ0HKEJ0ZpFwER8POwAEOmYilN0FsIKgDIm5QS9LUuL7dpmna8ys8ZZU-d91lWfVbfDjcOFSVPfYNPhsipK3NlNa73pem-xqfNRbL0NYVDO0Ykz62Av_uYUfcyflrOXaPH-_Dp7WESGciEjCgq0YNqS3EiuHXexUlQoojnRRqQ54SY1zGnBmYulpXJIBqCzNLU8V4JN0c3498vUztRFsmp6Xw-OyU-Rb8vvxNIhH7DhbGCvR7b1zba3oTvAVCqhiRACBurqXwpiBVyRve3tCGW-CcFbl7S-2hi_Swgk-_aTQ_vsFyLOc-s</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>204805816</pqid></control><display><type>article</type><title>The electrical conductivity of gabbro at high temperature and high pressure</title><source>Springer Nature</source><creator>Doujun, Wang ; Heping, Li ; Li, Yi ; Weigang, Zhang ; Congqiang, Liu ; Gengli, Suo ; Dongye, Ding</creator><creatorcontrib>Doujun, Wang ; Heping, Li ; Li, Yi ; Weigang, Zhang ; Congqiang, Liu ; Gengli, Suo ; Dongye, Ding</creatorcontrib><description>The electric conductivity of gabbro has been measured at 1.0-2.0 GPa and 320-700°C, and the conduction mechanism has been analyzed in terms of the impedance spectra. Experimental results indicated that the electric conductivity depends on the frequency of alternative current. Impedance arcs representing the conduction mechanism of grain interiors are displayed in the complex impedance plane, and the mechanism is dominated at high pressure. These arcs occur over the range of 10^sup 2^ -k × 10^sup 5^ Hz (k is the positive integer from 1 to 9). On the basis of our results and previous work, it is concluded that gabbro cannot form any high conductivity layer (HCL) in the middle-lower crust.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 1000-9426</identifier><identifier>ISSN: 2096-0956</identifier><identifier>EISSN: 1993-0364</identifier><identifier>EISSN: 2365-7499</identifier><identifier>DOI: 10.1007/BF02831090</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Conduction ; Conductivity ; Electric arcs ; Electrical conductivity ; Electrical resistivity ; Gabbro ; Geochemistry ; Geophysics ; High pressure ; High temperature ; Impedance</subject><ispartof>Acta geochimica, 2002-07, Vol.21 (3), p.252-257</ispartof><rights>Institute of Geochemistry, Chinese Academy of Sciences 2002</rights><rights>Institute of Geochemistry, Chinese Academy of Sciences 2002.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a2567-20809639e1da759f5f48826819519a6bd15aba3f9653f47e27007009cbbe5d863</citedby><cites>FETCH-LOGICAL-a2567-20809639e1da759f5f48826819519a6bd15aba3f9653f47e27007009cbbe5d863</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/zgdqhx-e/zgdqhx-e.jpg</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Doujun, Wang</creatorcontrib><creatorcontrib>Heping, Li</creatorcontrib><creatorcontrib>Li, Yi</creatorcontrib><creatorcontrib>Weigang, Zhang</creatorcontrib><creatorcontrib>Congqiang, Liu</creatorcontrib><creatorcontrib>Gengli, Suo</creatorcontrib><creatorcontrib>Dongye, Ding</creatorcontrib><title>The electrical conductivity of gabbro at high temperature and high pressure</title><title>Acta geochimica</title><description>The electric conductivity of gabbro has been measured at 1.0-2.0 GPa and 320-700°C, and the conduction mechanism has been analyzed in terms of the impedance spectra. Experimental results indicated that the electric conductivity depends on the frequency of alternative current. Impedance arcs representing the conduction mechanism of grain interiors are displayed in the complex impedance plane, and the mechanism is dominated at high pressure. These arcs occur over the range of 10^sup 2^ -k × 10^sup 5^ Hz (k is the positive integer from 1 to 9). On the basis of our results and previous work, it is concluded that gabbro cannot form any high conductivity layer (HCL) in the middle-lower crust.[PUBLICATION ABSTRACT]</description><subject>Conduction</subject><subject>Conductivity</subject><subject>Electric arcs</subject><subject>Electrical conductivity</subject><subject>Electrical resistivity</subject><subject>Gabbro</subject><subject>Geochemistry</subject><subject>Geophysics</subject><subject>High pressure</subject><subject>High temperature</subject><subject>Impedance</subject><issn>1000-9426</issn><issn>2096-0956</issn><issn>1993-0364</issn><issn>2365-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNp1kM1OwzAQhC0EEqVw4QksOIEUWNvx3xEqCohKXMo5chI7SdUmqZ0A5elJFaSeOO1q9O2OZhC6JHBHAOT94xyoYgQ0HKEJ0ZpFwER8POwAEOmYilN0FsIKgDIm5QS9LUuL7dpmna8ys8ZZU-d91lWfVbfDjcOFSVPfYNPhsipK3NlNa73pem-xqfNRbL0NYVDO0Ykz62Av_uYUfcyflrOXaPH-_Dp7WESGciEjCgq0YNqS3EiuHXexUlQoojnRRqQ54SY1zGnBmYulpXJIBqCzNLU8V4JN0c3498vUztRFsmp6Xw-OyU-Rb8vvxNIhH7DhbGCvR7b1zba3oTvAVCqhiRACBurqXwpiBVyRve3tCGW-CcFbl7S-2hi_Swgk-_aTQ_vsFyLOc-s</recordid><startdate>20020701</startdate><enddate>20020701</enddate><creator>Doujun, Wang</creator><creator>Heping, Li</creator><creator>Li, Yi</creator><creator>Weigang, Zhang</creator><creator>Congqiang, Liu</creator><creator>Gengli, Suo</creator><creator>Dongye, Ding</creator><general>Springer Nature B.V</general><general>Laboratory of the Earth' s Interior and Geofluids, Institute of Geochemistry, Chinese Academy of Sciences, Cruiyang 550002, China</general><general>Graduate School of Chinese Academy of Sciences, Beijing 100083, China%Laboratory of the Earth' s Interior and Geofluids, Institute of Geochemistry, Chinese Academy of Sciences, Cruiyang 550002, China%Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China %Oil University, Beijing 102200, China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20020701</creationdate><title>The electrical conductivity of gabbro at high temperature and high pressure</title><author>Doujun, Wang ; Heping, Li ; Li, Yi ; Weigang, Zhang ; Congqiang, Liu ; Gengli, Suo ; Dongye, Ding</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a2567-20809639e1da759f5f48826819519a6bd15aba3f9653f47e27007009cbbe5d863</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Conduction</topic><topic>Conductivity</topic><topic>Electric arcs</topic><topic>Electrical conductivity</topic><topic>Electrical resistivity</topic><topic>Gabbro</topic><topic>Geochemistry</topic><topic>Geophysics</topic><topic>High pressure</topic><topic>High temperature</topic><topic>Impedance</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Doujun, Wang</creatorcontrib><creatorcontrib>Heping, Li</creatorcontrib><creatorcontrib>Li, Yi</creatorcontrib><creatorcontrib>Weigang, Zhang</creatorcontrib><creatorcontrib>Congqiang, Liu</creatorcontrib><creatorcontrib>Gengli, Suo</creatorcontrib><creatorcontrib>Dongye, Ding</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Materials Research Database</collection><collection>Materials Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Acta geochimica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Doujun, Wang</au><au>Heping, Li</au><au>Li, Yi</au><au>Weigang, Zhang</au><au>Congqiang, Liu</au><au>Gengli, Suo</au><au>Dongye, Ding</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The electrical conductivity of gabbro at high temperature and high pressure</atitle><jtitle>Acta geochimica</jtitle><date>2002-07-01</date><risdate>2002</risdate><volume>21</volume><issue>3</issue><spage>252</spage><epage>257</epage><pages>252-257</pages><issn>1000-9426</issn><issn>2096-0956</issn><eissn>1993-0364</eissn><eissn>2365-7499</eissn><abstract>The electric conductivity of gabbro has been measured at 1.0-2.0 GPa and 320-700°C, and the conduction mechanism has been analyzed in terms of the impedance spectra. Experimental results indicated that the electric conductivity depends on the frequency of alternative current. Impedance arcs representing the conduction mechanism of grain interiors are displayed in the complex impedance plane, and the mechanism is dominated at high pressure. These arcs occur over the range of 10^sup 2^ -k × 10^sup 5^ Hz (k is the positive integer from 1 to 9). On the basis of our results and previous work, it is concluded that gabbro cannot form any high conductivity layer (HCL) in the middle-lower crust.[PUBLICATION ABSTRACT]</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1007/BF02831090</doi><tpages>6</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1000-9426 |
ispartof | Acta geochimica, 2002-07, Vol.21 (3), p.252-257 |
issn | 1000-9426 2096-0956 1993-0364 2365-7499 |
language | eng |
recordid | cdi_wanfang_journals_zgdqhx_e200203007 |
source | Springer Nature |
subjects | Conduction Conductivity Electric arcs Electrical conductivity Electrical resistivity Gabbro Geochemistry Geophysics High pressure High temperature Impedance |
title | The electrical conductivity of gabbro at high temperature and high pressure |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-04T03%3A51%3A25IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20electrical%20conductivity%20of%20gabbro%20at%20high%20temperature%20and%20high%20pressure&rft.jtitle=Acta%20geochimica&rft.au=Doujun,%20Wang&rft.date=2002-07-01&rft.volume=21&rft.issue=3&rft.spage=252&rft.epage=257&rft.pages=252-257&rft.issn=1000-9426&rft.eissn=1993-0364&rft_id=info:doi/10.1007/BF02831090&rft_dat=%3Cwanfang_jour_proqu%3Ezgdqhx_e200203007%3C/wanfang_jour_proqu%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a2567-20809639e1da759f5f48826819519a6bd15aba3f9653f47e27007009cbbe5d863%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=204805816&rft_id=info:pmid/&rft_wanfj_id=zgdqhx_e200203007&rfr_iscdi=true |