Loading…
Mud and fluid migration in active mud volcanoes in Azerbaijan
Mud volcanic eruptions in Azerbaijan normally last for less than a few hours, and are characterized by vigorous extrusion of mud breccias, hydrocarbon gases, and waters. Recent fieldwork and mapping on four active mud volcanoes show that dormant period activity ranges from quiet to vigorous flow of...
Saved in:
Published in: | Geo-marine letters 2003-12, Vol.23 (3-4), p.258-268 |
---|---|
Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | 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-a359t-a8782f89c58d4097dfbf0fba27fedbd6f993c96b94ea80f21cf01a5aa4a96fe23 |
---|---|
cites | |
container_end_page | 268 |
container_issue | 3-4 |
container_start_page | 258 |
container_title | Geo-marine letters |
container_volume | 23 |
creator | Planke, S Svensen, H Hovland, M Banks, DA Jamtveit, B |
description | Mud volcanic eruptions in Azerbaijan normally last for less than a few hours, and are characterized by vigorous extrusion of mud breccias, hydrocarbon gases, and waters. Recent fieldwork and mapping on four active mud volcanoes show that dormant period activity ranges from quiet to vigorous flow of mud and fluids. Geochemical analyses of expelled waters show a wide range in solute concentrations, suggesting the existence of a complex plumbing system. The mud and fluids have a deep origin, but are sometimes stored in intermediate-depth mud chambers. A mixing model between deep-seated saline waters and shallow meteoric water is proposed. |
doi_str_mv | 10.1007/s00367-003-0152-z |
format | article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_17679323</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>677683001</sourcerecordid><originalsourceid>FETCH-LOGICAL-a359t-a8782f89c58d4097dfbf0fba27fedbd6f993c96b94ea80f21cf01a5aa4a96fe23</originalsourceid><addsrcrecordid>eNp9kEtLAzEUhYMoWKs_wN3gQtxEb5KZZLJwUYovqLjRdbiTSSRlHjWZKdhf75S6cuHmXDh8XDgfIZcMbhmAuksAQio6JQVWcLo7IjOWC04ZK9QxmQFXkkIu4ZScpbQGgFyVbEbuX8c6w67OfDOGOmvDZ8Qh9F0WugztELYuaydi2zcWu96lfb_YuVhhWGN3Tk48Nsld_N45-Xh8eF8-09Xb08tysaIoCj1QLFXJfaltUdY5aFX7yoOvkCvv6qqWXmthtax07rAEz5n1wLBAzFFL77iYk-vD303sv0aXBtOGZF3TYOf6MRmmpNKCiwm8-R8sOMuBiUnNnFz9Qdf9GLtphuEceKm4lBPEDpCNfUrRebOJocX4bRiYvXhzEG-mNHvxZid-ALSodYQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>220287266</pqid></control><display><type>article</type><title>Mud and fluid migration in active mud volcanoes in Azerbaijan</title><source>Springer Nature</source><creator>Planke, S ; Svensen, H ; Hovland, M ; Banks, DA ; Jamtveit, B</creator><creatorcontrib>Planke, S ; Svensen, H ; Hovland, M ; Banks, DA ; Jamtveit, B</creatorcontrib><description>Mud volcanic eruptions in Azerbaijan normally last for less than a few hours, and are characterized by vigorous extrusion of mud breccias, hydrocarbon gases, and waters. Recent fieldwork and mapping on four active mud volcanoes show that dormant period activity ranges from quiet to vigorous flow of mud and fluids. Geochemical analyses of expelled waters show a wide range in solute concentrations, suggesting the existence of a complex plumbing system. The mud and fluids have a deep origin, but are sometimes stored in intermediate-depth mud chambers. A mixing model between deep-seated saline waters and shallow meteoric water is proposed.</description><identifier>ISSN: 0276-0460</identifier><identifier>EISSN: 1432-1157</identifier><identifier>DOI: 10.1007/s00367-003-0152-z</identifier><language>eng</language><publisher>Heidelberg: Springer Nature B.V</publisher><subject>Fieldwork ; Fluids ; Landslides & mudslides ; Marine ; Meteoric water ; Mudflows ; Volcanic eruptions ; Volcanoes</subject><ispartof>Geo-marine letters, 2003-12, Vol.23 (3-4), p.258-268</ispartof><rights>Copyright Springer-Verlag 2003</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a359t-a8782f89c58d4097dfbf0fba27fedbd6f993c96b94ea80f21cf01a5aa4a96fe23</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Planke, S</creatorcontrib><creatorcontrib>Svensen, H</creatorcontrib><creatorcontrib>Hovland, M</creatorcontrib><creatorcontrib>Banks, DA</creatorcontrib><creatorcontrib>Jamtveit, B</creatorcontrib><title>Mud and fluid migration in active mud volcanoes in Azerbaijan</title><title>Geo-marine letters</title><description>Mud volcanic eruptions in Azerbaijan normally last for less than a few hours, and are characterized by vigorous extrusion of mud breccias, hydrocarbon gases, and waters. Recent fieldwork and mapping on four active mud volcanoes show that dormant period activity ranges from quiet to vigorous flow of mud and fluids. Geochemical analyses of expelled waters show a wide range in solute concentrations, suggesting the existence of a complex plumbing system. The mud and fluids have a deep origin, but are sometimes stored in intermediate-depth mud chambers. A mixing model between deep-seated saline waters and shallow meteoric water is proposed.</description><subject>Fieldwork</subject><subject>Fluids</subject><subject>Landslides & mudslides</subject><subject>Marine</subject><subject>Meteoric water</subject><subject>Mudflows</subject><subject>Volcanic eruptions</subject><subject>Volcanoes</subject><issn>0276-0460</issn><issn>1432-1157</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNp9kEtLAzEUhYMoWKs_wN3gQtxEb5KZZLJwUYovqLjRdbiTSSRlHjWZKdhf75S6cuHmXDh8XDgfIZcMbhmAuksAQio6JQVWcLo7IjOWC04ZK9QxmQFXkkIu4ZScpbQGgFyVbEbuX8c6w67OfDOGOmvDZ8Qh9F0WugztELYuaydi2zcWu96lfb_YuVhhWGN3Tk48Nsld_N45-Xh8eF8-09Xb08tysaIoCj1QLFXJfaltUdY5aFX7yoOvkCvv6qqWXmthtax07rAEz5n1wLBAzFFL77iYk-vD303sv0aXBtOGZF3TYOf6MRmmpNKCiwm8-R8sOMuBiUnNnFz9Qdf9GLtphuEceKm4lBPEDpCNfUrRebOJocX4bRiYvXhzEG-mNHvxZid-ALSodYQ</recordid><startdate>20031201</startdate><enddate>20031201</enddate><creator>Planke, S</creator><creator>Svensen, H</creator><creator>Hovland, M</creator><creator>Banks, DA</creator><creator>Jamtveit, B</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</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>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope></search><sort><creationdate>20031201</creationdate><title>Mud and fluid migration in active mud volcanoes in Azerbaijan</title><author>Planke, S ; Svensen, H ; Hovland, M ; Banks, DA ; Jamtveit, B</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a359t-a8782f89c58d4097dfbf0fba27fedbd6f993c96b94ea80f21cf01a5aa4a96fe23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Fieldwork</topic><topic>Fluids</topic><topic>Landslides & mudslides</topic><topic>Marine</topic><topic>Meteoric water</topic><topic>Mudflows</topic><topic>Volcanic eruptions</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Planke, S</creatorcontrib><creatorcontrib>Svensen, H</creatorcontrib><creatorcontrib>Hovland, M</creatorcontrib><creatorcontrib>Banks, DA</creatorcontrib><creatorcontrib>Jamtveit, B</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</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</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>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</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>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>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><jtitle>Geo-marine letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Planke, S</au><au>Svensen, H</au><au>Hovland, M</au><au>Banks, DA</au><au>Jamtveit, B</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mud and fluid migration in active mud volcanoes in Azerbaijan</atitle><jtitle>Geo-marine letters</jtitle><date>2003-12-01</date><risdate>2003</risdate><volume>23</volume><issue>3-4</issue><spage>258</spage><epage>268</epage><pages>258-268</pages><issn>0276-0460</issn><eissn>1432-1157</eissn><abstract>Mud volcanic eruptions in Azerbaijan normally last for less than a few hours, and are characterized by vigorous extrusion of mud breccias, hydrocarbon gases, and waters. Recent fieldwork and mapping on four active mud volcanoes show that dormant period activity ranges from quiet to vigorous flow of mud and fluids. Geochemical analyses of expelled waters show a wide range in solute concentrations, suggesting the existence of a complex plumbing system. The mud and fluids have a deep origin, but are sometimes stored in intermediate-depth mud chambers. A mixing model between deep-seated saline waters and shallow meteoric water is proposed.</abstract><cop>Heidelberg</cop><pub>Springer Nature B.V</pub><doi>10.1007/s00367-003-0152-z</doi><tpages>11</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0276-0460 |
ispartof | Geo-marine letters, 2003-12, Vol.23 (3-4), p.258-268 |
issn | 0276-0460 1432-1157 |
language | eng |
recordid | cdi_proquest_miscellaneous_17679323 |
source | Springer Nature |
subjects | Fieldwork Fluids Landslides & mudslides Marine Meteoric water Mudflows Volcanic eruptions Volcanoes |
title | Mud and fluid migration in active mud volcanoes in Azerbaijan |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-26T17%3A20%3A57IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Mud%20and%20fluid%20migration%20in%20active%20mud%20volcanoes%20in%20Azerbaijan&rft.jtitle=Geo-marine%20letters&rft.au=Planke,%20S&rft.date=2003-12-01&rft.volume=23&rft.issue=3-4&rft.spage=258&rft.epage=268&rft.pages=258-268&rft.issn=0276-0460&rft.eissn=1432-1157&rft_id=info:doi/10.1007/s00367-003-0152-z&rft_dat=%3Cproquest_cross%3E677683001%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a359t-a8782f89c58d4097dfbf0fba27fedbd6f993c96b94ea80f21cf01a5aa4a96fe23%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=220287266&rft_id=info:pmid/&rfr_iscdi=true |