Loading…

Petrological and geochemical characteristics of Plio-Pleistocene Volcanics from Ponza Island (Tyrrhenian Sea, Italy)

Volcanic rocks on Ponza Island (Tyrrhenian Sea, central Italy) consist of Pliocene submarine rhyolites and Pleistocene subaerial trachyte and comendite lavas. Chemical variations and the homogeneous Sr and Nd isotopic signatures within the analyzed Pliocene rocks are ascribed to crystal fractionatio...

Full description

Saved in:
Bibliographic Details
Published in:Mineralogy and petrology 2002-01, Vol.74 (1), p.75-94
Main Authors: Conte, A M, Dolfi, D
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-a322t-8560d8754066014e92d9491016149ad74c85a052b5501f92f8ab23fcf871d95d3
cites
container_end_page 94
container_issue 1
container_start_page 75
container_title Mineralogy and petrology
container_volume 74
creator Conte, A M
Dolfi, D
description Volcanic rocks on Ponza Island (Tyrrhenian Sea, central Italy) consist of Pliocene submarine rhyolites and Pleistocene subaerial trachyte and comendite lavas. Chemical variations and the homogeneous Sr and Nd isotopic signatures within the analyzed Pliocene rocks are ascribed to crystal fractionation. The absolute isotopic values, however, indicate the important role of a crustal component in the origin of these magmas. The very high-silica rocks were probably derived from a superimposed mechanism which may have been connected to the ascent of hydrothermal magmatic fluids. Compositional and 87Sr/86Sr variations at constant 143Nd/144Nd values in the Pleistocene rocks are likely due to fractionation of the observed phenocryst assemblage, possibly coupled with minor crustal interaction. These processes, however, cannot account for the extreme enrichment of many incompatible trace elements in the comendites. Some evidence suggests the influence of a halogen- and/or CO2-rich volatile phase. [PUBLICATION ABSTRACT]
doi_str_mv 10.1007/s710-002-8216-6
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1238121349</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1238121349</sourcerecordid><originalsourceid>FETCH-LOGICAL-a322t-8560d8754066014e92d9491016149ad74c85a052b5501f92f8ab23fcf871d95d3</originalsourceid><addsrcrecordid>eNpdkU1LAzEQhoMoWKtnr8FTBdfOZL-yRxE_CgUXrF5Dmk3aLemmJttD_fVmrSdPw8z7MLzwEHKNcI8A5TSUCAkASzjDIilOyAizlCeIBT8lI6jSmJbAz8lFCBsA4DnHEelr3Xtn3apV0lLZNXSlnVrr7e-u1tJL1Wvfhr5VgTpDa9u6pLY6XpzSnaafzirZDanxbktr131LOgt2-DVZHLxf666VHX3X8o7OemkPt5fkzEgb9NXfHJOP56fF42syf3uZPT7ME5ky1ic8L6DhZZ5BUQBmumJNlVUIWGBWyabMFM8l5GyZ54CmYobLJUuNMrzEpsqbdEwmx7877772OvRi2walbeym3T4IZClHhmlWRfTmH7pxe9_FdoKxyMQWGKHpEVLeheC1ETvfbqU_CAQxSBCDBBEliEGCKNIf0Cl45A</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>221217541</pqid></control><display><type>article</type><title>Petrological and geochemical characteristics of Plio-Pleistocene Volcanics from Ponza Island (Tyrrhenian Sea, Italy)</title><source>Springer Link</source><creator>Conte, A M ; Dolfi, D</creator><creatorcontrib>Conte, A M ; Dolfi, D</creatorcontrib><description>Volcanic rocks on Ponza Island (Tyrrhenian Sea, central Italy) consist of Pliocene submarine rhyolites and Pleistocene subaerial trachyte and comendite lavas. Chemical variations and the homogeneous Sr and Nd isotopic signatures within the analyzed Pliocene rocks are ascribed to crystal fractionation. The absolute isotopic values, however, indicate the important role of a crustal component in the origin of these magmas. The very high-silica rocks were probably derived from a superimposed mechanism which may have been connected to the ascent of hydrothermal magmatic fluids. Compositional and 87Sr/86Sr variations at constant 143Nd/144Nd values in the Pleistocene rocks are likely due to fractionation of the observed phenocryst assemblage, possibly coupled with minor crustal interaction. These processes, however, cannot account for the extreme enrichment of many incompatible trace elements in the comendites. Some evidence suggests the influence of a halogen- and/or CO2-rich volatile phase. [PUBLICATION ABSTRACT]</description><identifier>ISSN: 0930-0708</identifier><identifier>EISSN: 1438-1168</identifier><identifier>DOI: 10.1007/s710-002-8216-6</identifier><language>eng</language><publisher>Wien: Springer Nature B.V</publisher><subject>Carbon dioxide ; Fractionation ; Geochemistry ; Islands ; Metamorphic rocks ; Petrology ; Pleistocene ; Pliocene ; Silica ; Trace elements ; Volcanic rocks ; Volcanoes</subject><ispartof>Mineralogy and petrology, 2002-01, Vol.74 (1), p.75-94</ispartof><rights>Copyright Springer-Verlag 2002</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a322t-8560d8754066014e92d9491016149ad74c85a052b5501f92f8ab23fcf871d95d3</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>Conte, A M</creatorcontrib><creatorcontrib>Dolfi, D</creatorcontrib><title>Petrological and geochemical characteristics of Plio-Pleistocene Volcanics from Ponza Island (Tyrrhenian Sea, Italy)</title><title>Mineralogy and petrology</title><description>Volcanic rocks on Ponza Island (Tyrrhenian Sea, central Italy) consist of Pliocene submarine rhyolites and Pleistocene subaerial trachyte and comendite lavas. Chemical variations and the homogeneous Sr and Nd isotopic signatures within the analyzed Pliocene rocks are ascribed to crystal fractionation. The absolute isotopic values, however, indicate the important role of a crustal component in the origin of these magmas. The very high-silica rocks were probably derived from a superimposed mechanism which may have been connected to the ascent of hydrothermal magmatic fluids. Compositional and 87Sr/86Sr variations at constant 143Nd/144Nd values in the Pleistocene rocks are likely due to fractionation of the observed phenocryst assemblage, possibly coupled with minor crustal interaction. These processes, however, cannot account for the extreme enrichment of many incompatible trace elements in the comendites. Some evidence suggests the influence of a halogen- and/or CO2-rich volatile phase. [PUBLICATION ABSTRACT]</description><subject>Carbon dioxide</subject><subject>Fractionation</subject><subject>Geochemistry</subject><subject>Islands</subject><subject>Metamorphic rocks</subject><subject>Petrology</subject><subject>Pleistocene</subject><subject>Pliocene</subject><subject>Silica</subject><subject>Trace elements</subject><subject>Volcanic rocks</subject><subject>Volcanoes</subject><issn>0930-0708</issn><issn>1438-1168</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNpdkU1LAzEQhoMoWKtnr8FTBdfOZL-yRxE_CgUXrF5Dmk3aLemmJttD_fVmrSdPw8z7MLzwEHKNcI8A5TSUCAkASzjDIilOyAizlCeIBT8lI6jSmJbAz8lFCBsA4DnHEelr3Xtn3apV0lLZNXSlnVrr7e-u1tJL1Wvfhr5VgTpDa9u6pLY6XpzSnaafzirZDanxbktr131LOgt2-DVZHLxf666VHX3X8o7OemkPt5fkzEgb9NXfHJOP56fF42syf3uZPT7ME5ky1ic8L6DhZZ5BUQBmumJNlVUIWGBWyabMFM8l5GyZ54CmYobLJUuNMrzEpsqbdEwmx7877772OvRi2walbeym3T4IZClHhmlWRfTmH7pxe9_FdoKxyMQWGKHpEVLeheC1ETvfbqU_CAQxSBCDBBEliEGCKNIf0Cl45A</recordid><startdate>20020101</startdate><enddate>20020101</enddate><creator>Conte, A M</creator><creator>Dolfi, D</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7TN</scope></search><sort><creationdate>20020101</creationdate><title>Petrological and geochemical characteristics of Plio-Pleistocene Volcanics from Ponza Island (Tyrrhenian Sea, Italy)</title><author>Conte, A M ; Dolfi, D</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a322t-8560d8754066014e92d9491016149ad74c85a052b5501f92f8ab23fcf871d95d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Carbon dioxide</topic><topic>Fractionation</topic><topic>Geochemistry</topic><topic>Islands</topic><topic>Metamorphic rocks</topic><topic>Petrology</topic><topic>Pleistocene</topic><topic>Pliocene</topic><topic>Silica</topic><topic>Trace elements</topic><topic>Volcanic rocks</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Conte, A M</creatorcontrib><creatorcontrib>Dolfi, D</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</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>Research Library (Alumni Edition)</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Earth, Atmospheric &amp; Aquatic Science</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Materials Research Database</collection><collection>ProQuest Materials Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>ProQuest research library</collection><collection>ProQuest Science Journals</collection><collection>ProQuest Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Environmental Science Database</collection><collection>ProQuest Earth, Atmospheric &amp; 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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Oceanic Abstracts</collection><jtitle>Mineralogy and petrology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Conte, A M</au><au>Dolfi, D</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Petrological and geochemical characteristics of Plio-Pleistocene Volcanics from Ponza Island (Tyrrhenian Sea, Italy)</atitle><jtitle>Mineralogy and petrology</jtitle><date>2002-01-01</date><risdate>2002</risdate><volume>74</volume><issue>1</issue><spage>75</spage><epage>94</epage><pages>75-94</pages><issn>0930-0708</issn><eissn>1438-1168</eissn><abstract>Volcanic rocks on Ponza Island (Tyrrhenian Sea, central Italy) consist of Pliocene submarine rhyolites and Pleistocene subaerial trachyte and comendite lavas. Chemical variations and the homogeneous Sr and Nd isotopic signatures within the analyzed Pliocene rocks are ascribed to crystal fractionation. The absolute isotopic values, however, indicate the important role of a crustal component in the origin of these magmas. The very high-silica rocks were probably derived from a superimposed mechanism which may have been connected to the ascent of hydrothermal magmatic fluids. Compositional and 87Sr/86Sr variations at constant 143Nd/144Nd values in the Pleistocene rocks are likely due to fractionation of the observed phenocryst assemblage, possibly coupled with minor crustal interaction. These processes, however, cannot account for the extreme enrichment of many incompatible trace elements in the comendites. Some evidence suggests the influence of a halogen- and/or CO2-rich volatile phase. [PUBLICATION ABSTRACT]</abstract><cop>Wien</cop><pub>Springer Nature B.V</pub><doi>10.1007/s710-002-8216-6</doi><tpages>20</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0930-0708
ispartof Mineralogy and petrology, 2002-01, Vol.74 (1), p.75-94
issn 0930-0708
1438-1168
language eng
recordid cdi_proquest_miscellaneous_1238121349
source Springer Link
subjects Carbon dioxide
Fractionation
Geochemistry
Islands
Metamorphic rocks
Petrology
Pleistocene
Pliocene
Silica
Trace elements
Volcanic rocks
Volcanoes
title Petrological and geochemical characteristics of Plio-Pleistocene Volcanics from Ponza Island (Tyrrhenian Sea, Italy)
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-07T20%3A47%3A24IST&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=Petrological%20and%20geochemical%20characteristics%20of%20Plio-Pleistocene%20Volcanics%20from%20Ponza%20Island%20(Tyrrhenian%20Sea,%20Italy)&rft.jtitle=Mineralogy%20and%20petrology&rft.au=Conte,%20A%20M&rft.date=2002-01-01&rft.volume=74&rft.issue=1&rft.spage=75&rft.epage=94&rft.pages=75-94&rft.issn=0930-0708&rft.eissn=1438-1168&rft_id=info:doi/10.1007/s710-002-8216-6&rft_dat=%3Cproquest_cross%3E1238121349%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a322t-8560d8754066014e92d9491016149ad74c85a052b5501f92f8ab23fcf871d95d3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=221217541&rft_id=info:pmid/&rfr_iscdi=true