Study on Zircon LA-ICP-MS U-Pb Dating and Sr-Nd Isotope of the Guposhan Granite in Guangxi

Study on Zircon LA-ICP-MS U-Pb Dating and Sr-Nd Isotope of the Guposhan Granite in Guangxi

Zircon U-Pb dating with the LA-ICP-MS method was applied to determining the ages of different units of the Guposhan granite, among which the east Guposhan unit is 160. 8 plus/minus 1. 6 Ma, the west Guposhan unit is 165. 0+/-1. 9 Ma, and the Lisong unit is 163. 0+1. 3 Ma in age. It is worth noticing...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Dìzhìxué bào 2006-01, Vol.80 (4), p.553-559
Hauptverfasser: Gu, Shengyan, Hua, Renmin, Qi, Huawen
Format: Artikel
Sprache:chi
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 559
container_issue 4
container_start_page 553
container_title Dìzhìxué bào
container_volume 80
creator Gu, Shengyan
Hua, Renmin
Qi, Huawen
description Zircon U-Pb dating with the LA-ICP-MS method was applied to determining the ages of different units of the Guposhan granite, among which the east Guposhan unit is 160. 8 plus/minus 1. 6 Ma, the west Guposhan unit is 165. 0+/-1. 9 Ma, and the Lisong unit is 163. 0+1. 3 Ma in age. It is worth noticing that the ages of the three units are very similar to each other within the analytical error. It thus proves that the whole Guposhan granite was formed in the same age. They are products of large-scale magmatism of crust-remelting granitoids in the first stage of the middle Yanshanian Period in South China. Though forming in the same age, the three units have differences in petrological and geochemical characteristics. Besides the differences in major, trace and rare earth elements, they are distinct in their Rb-Sr and Sm-Nd isotopic compositions. The east unit, Lisong unit and its enclaves have a similar ('Sr/'Sr); value of 0. 70643 and average eNd (t) (-3. 03) , indicating that more mantle materials participated
format Article
fullrecord <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_miscellaneous_29562682</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>29562682</sourcerecordid><originalsourceid>FETCH-proquest_miscellaneous_295626823</originalsourceid><addsrcrecordid>eNqNyrEOgjAUQNEOmkiUf3iTW5OCWnA0qEiixgRdWEiVok2wRV6b6N_L4Ac4nTvcAfEYYwFdREE0Ij6iurJwxuecs9gjRW5d9QGjoVDdrWe_ollyooccLvR0hbWwSt9B6Aryjh4ryNBY00owNdiHhNS1Bh9CQ9oJrawE1acT-v5WEzKsRYPS_zkm0-3mnOxo25mXk2jLp8KbbBqhpXFYhssFD3kczv4ev2VJQ1c</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>29562682</pqid></control><display><type>article</type><title>Study on Zircon LA-ICP-MS U-Pb Dating and Sr-Nd Isotope of the Guposhan Granite in Guangxi</title><source>Alma/SFX Local Collection</source><creator>Gu, Shengyan ; Hua, Renmin ; Qi, Huawen</creator><creatorcontrib>Gu, Shengyan ; Hua, Renmin ; Qi, Huawen</creatorcontrib><description>Zircon U-Pb dating with the LA-ICP-MS method was applied to determining the ages of different units of the Guposhan granite, among which the east Guposhan unit is 160. 8 plus/minus 1. 6 Ma, the west Guposhan unit is 165. 0+/-1. 9 Ma, and the Lisong unit is 163. 0+1. 3 Ma in age. It is worth noticing that the ages of the three units are very similar to each other within the analytical error. It thus proves that the whole Guposhan granite was formed in the same age. They are products of large-scale magmatism of crust-remelting granitoids in the first stage of the middle Yanshanian Period in South China. Though forming in the same age, the three units have differences in petrological and geochemical characteristics. Besides the differences in major, trace and rare earth elements, they are distinct in their Rb-Sr and Sm-Nd isotopic compositions. The east unit, Lisong unit and its enclaves have a similar ('Sr/'Sr); value of 0. 70643 and average eNd (t) (-3. 03) , indicating that more mantle materials participated</description><identifier>ISSN: 0001-5717</identifier><language>chi</language><ispartof>Dìzhìxué bào, 2006-01, Vol.80 (4), p.553-559</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>314,777,781</link.rule.ids></links><search><creatorcontrib>Gu, Shengyan</creatorcontrib><creatorcontrib>Hua, Renmin</creatorcontrib><creatorcontrib>Qi, Huawen</creatorcontrib><title>Study on Zircon LA-ICP-MS U-Pb Dating and Sr-Nd Isotope of the Guposhan Granite in Guangxi</title><title>Dìzhìxué bào</title><description>Zircon U-Pb dating with the LA-ICP-MS method was applied to determining the ages of different units of the Guposhan granite, among which the east Guposhan unit is 160. 8 plus/minus 1. 6 Ma, the west Guposhan unit is 165. 0+/-1. 9 Ma, and the Lisong unit is 163. 0+1. 3 Ma in age. It is worth noticing that the ages of the three units are very similar to each other within the analytical error. It thus proves that the whole Guposhan granite was formed in the same age. They are products of large-scale magmatism of crust-remelting granitoids in the first stage of the middle Yanshanian Period in South China. Though forming in the same age, the three units have differences in petrological and geochemical characteristics. Besides the differences in major, trace and rare earth elements, they are distinct in their Rb-Sr and Sm-Nd isotopic compositions. The east unit, Lisong unit and its enclaves have a similar ('Sr/'Sr); value of 0. 70643 and average eNd (t) (-3. 03) , indicating that more mantle materials participated</description><issn>0001-5717</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqNyrEOgjAUQNEOmkiUf3iTW5OCWnA0qEiixgRdWEiVok2wRV6b6N_L4Ac4nTvcAfEYYwFdREE0Ij6iurJwxuecs9gjRW5d9QGjoVDdrWe_ollyooccLvR0hbWwSt9B6Aryjh4ryNBY00owNdiHhNS1Bh9CQ9oJrawE1acT-v5WEzKsRYPS_zkm0-3mnOxo25mXk2jLp8KbbBqhpXFYhssFD3kczv4ev2VJQ1c</recordid><startdate>20060101</startdate><enddate>20060101</enddate><creator>Gu, Shengyan</creator><creator>Hua, Renmin</creator><creator>Qi, Huawen</creator><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20060101</creationdate><title>Study on Zircon LA-ICP-MS U-Pb Dating and Sr-Nd Isotope of the Guposhan Granite in Guangxi</title><author>Gu, Shengyan ; Hua, Renmin ; Qi, Huawen</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-proquest_miscellaneous_295626823</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi</language><creationdate>2006</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gu, Shengyan</creatorcontrib><creatorcontrib>Hua, Renmin</creatorcontrib><creatorcontrib>Qi, Huawen</creatorcontrib><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Dìzhìxué bào</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gu, Shengyan</au><au>Hua, Renmin</au><au>Qi, Huawen</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Study on Zircon LA-ICP-MS U-Pb Dating and Sr-Nd Isotope of the Guposhan Granite in Guangxi</atitle><jtitle>Dìzhìxué bào</jtitle><date>2006-01-01</date><risdate>2006</risdate><volume>80</volume><issue>4</issue><spage>553</spage><epage>559</epage><pages>553-559</pages><issn>0001-5717</issn><abstract>Zircon U-Pb dating with the LA-ICP-MS method was applied to determining the ages of different units of the Guposhan granite, among which the east Guposhan unit is 160. 8 plus/minus 1. 6 Ma, the west Guposhan unit is 165. 0+/-1. 9 Ma, and the Lisong unit is 163. 0+1. 3 Ma in age. It is worth noticing that the ages of the three units are very similar to each other within the analytical error. It thus proves that the whole Guposhan granite was formed in the same age. They are products of large-scale magmatism of crust-remelting granitoids in the first stage of the middle Yanshanian Period in South China. Though forming in the same age, the three units have differences in petrological and geochemical characteristics. Besides the differences in major, trace and rare earth elements, they are distinct in their Rb-Sr and Sm-Nd isotopic compositions. The east unit, Lisong unit and its enclaves have a similar ('Sr/'Sr); value of 0. 70643 and average eNd (t) (-3. 03) , indicating that more mantle materials participated</abstract></addata></record>
fulltext fulltext
identifier ISSN: 0001-5717
ispartof Dìzhìxué bào, 2006-01, Vol.80 (4), p.553-559
issn 0001-5717
language chi
recordid cdi_proquest_miscellaneous_29562682
source Alma/SFX Local Collection
title Study on Zircon LA-ICP-MS U-Pb Dating and Sr-Nd Isotope of the Guposhan Granite in Guangxi
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-20T19%3A53%3A26IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Study%20on%20Zircon%20LA-ICP-MS%20U-Pb%20Dating%20and%20Sr-Nd%20Isotope%20of%20the%20Guposhan%20Granite%20in%20Guangxi&rft.jtitle=D%C3%ACzh%C3%ACxu%C3%A9%20b%C3%A0o&rft.au=Gu,%20Shengyan&rft.date=2006-01-01&rft.volume=80&rft.issue=4&rft.spage=553&rft.epage=559&rft.pages=553-559&rft.issn=0001-5717&rft_id=info:doi/&rft_dat=%3Cproquest%3E29562682%3C/proquest%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=29562682&rft_id=info:pmid/&rfr_iscdi=true