Geochemistry of Carboniferous Sandstones （Sardar Formation）, East-Central Iran： Implication for Provenance and Tectonic Setting

Geochemical analysis of sandstones from the Sardar Formation （from two stratigraphic successions） in east-central Iran were used for identification of geochemical characterization of sandstones, provenance and tectonic setting. Sandstones in the two lithostratigraphic successions have similar chemic...

Full description

Saved in:
Bibliographic Details
Published in:地质学报：英文版 2012, Vol.86 (5), p.1200-1210
Main Author: Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE
Format: Article
Language:English
Subjects:
伊朗
地球化学分析
地球化学特征
构造环境
物源
石炭纪
砂岩
被动大陆边缘
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by
cites
container_end_page 1210
container_issue 5
container_start_page 1200
container_title 地质学报：英文版
container_volume 86
creator Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE
description Geochemical analysis of sandstones from the Sardar Formation （from two stratigraphic successions） in east-central Iran were used for identification of geochemical characterization of sandstones, provenance and tectonic setting. Sandstones in the two lithostratigraphic successions have similar chemical compositions suggesting a common provenance. Bulk-rock geochemistry analysis of Carboniferous sandstones from Sardar Formation indicates that they are mainly quartz dominated and are classified as quartzarenites, sublitharenites and subarkoses, derived from acid igneous to intermediate igneous rocks. Discrimination function analysis indicates that the sandstones of Sardar Formation were derived from quartzose sedimentary provenance in a recycled orogenic setting. Also, major and trace elements in sandstones of Sardar Formation （e.g., K2O/Na2O vs. SiO2 ） indicate deposition in a stable passive continental margin （PM）. Chemical index of alteration （CIA） for these rocks （65%） suggests a moderate to relatively high degree of weathering in the source area.
format article
fullrecord <record><control><sourceid>chongqing</sourceid><recordid>TN_cdi_chongqing_primary_43766270</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>43766270</cqvip_id><sourcerecordid>43766270</sourcerecordid><originalsourceid>FETCH-chongqing_primary_437662703</originalsourceid><addsrcrecordid>eNqNjE1qAkEQRhtJQPNzh8o-Az1q95D1oIm7wLiXSlujHWa6THUn4AECyRU8i3fyCmnEA2T1PT4eb6BGZWVMYavx9Cqz1rp4MqUZqpsY37W2xpZmpL6fid2Weh-T7IFbqFHeOPiWhD8jNBjWMXGgCKfjT4OyRoE5S4_Jczgdfx9hhjEVNYUk2MFCML8HWPS7zruzBC0LvAp_UcDgCHIRluRy1DtoKCUfNnfqusUu0v1lb9XDfLasXwq35bD5yMZqJ75H2a-mk8racaUn_3H-ACrJVlc</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Geochemistry of Carboniferous Sandstones （Sardar Formation）, East-Central Iran： Implication for Provenance and Tectonic Setting</title><source>Wiley-Blackwell Read &amp; Publish Collection</source><creator>Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE</creator><creatorcontrib>Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE</creatorcontrib><description>Geochemical analysis of sandstones from the Sardar Formation （from two stratigraphic successions） in east-central Iran were used for identification of geochemical characterization of sandstones, provenance and tectonic setting. Sandstones in the two lithostratigraphic successions have similar chemical compositions suggesting a common provenance. Bulk-rock geochemistry analysis of Carboniferous sandstones from Sardar Formation indicates that they are mainly quartz dominated and are classified as quartzarenites, sublitharenites and subarkoses, derived from acid igneous to intermediate igneous rocks. Discrimination function analysis indicates that the sandstones of Sardar Formation were derived from quartzose sedimentary provenance in a recycled orogenic setting. Also, major and trace elements in sandstones of Sardar Formation （e.g., K2O/Na2O vs. SiO2 ） indicate deposition in a stable passive continental margin （PM）. Chemical index of alteration （CIA） for these rocks （65%） suggests a moderate to relatively high degree of weathering in the source area.</description><identifier>ISSN: 1000-9515</identifier><identifier>EISSN: 1755-6724</identifier><language>eng</language><subject>伊朗 ; 地球化学分析 ; 地球化学特征 ; 构造环境 ; 物源 ; 石炭纪 ; 砂岩 ; 被动大陆边缘</subject><ispartof>地质学报：英文版, 2012, Vol.86 (5), p.1200-1210</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/86253X/86253X.jpg</thumbnail><link.rule.ids>314,776,780,4010</link.rule.ids></links><search><creatorcontrib>Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE</creatorcontrib><title>Geochemistry of Carboniferous Sandstones （Sardar Formation）, East-Central Iran： Implication for Provenance and Tectonic Setting</title><title>地质学报：英文版</title><addtitle>Acta Geologica Sinica</addtitle><description>Geochemical analysis of sandstones from the Sardar Formation （from two stratigraphic successions） in east-central Iran were used for identification of geochemical characterization of sandstones, provenance and tectonic setting. Sandstones in the two lithostratigraphic successions have similar chemical compositions suggesting a common provenance. Bulk-rock geochemistry analysis of Carboniferous sandstones from Sardar Formation indicates that they are mainly quartz dominated and are classified as quartzarenites, sublitharenites and subarkoses, derived from acid igneous to intermediate igneous rocks. Discrimination function analysis indicates that the sandstones of Sardar Formation were derived from quartzose sedimentary provenance in a recycled orogenic setting. Also, major and trace elements in sandstones of Sardar Formation （e.g., K2O/Na2O vs. SiO2 ） indicate deposition in a stable passive continental margin （PM）. Chemical index of alteration （CIA） for these rocks （65%） suggests a moderate to relatively high degree of weathering in the source area.</description><subject>伊朗</subject><subject>地球化学分析</subject><subject>地球化学特征</subject><subject>构造环境</subject><subject>物源</subject><subject>石炭纪</subject><subject>砂岩</subject><subject>被动大陆边缘</subject><issn>1000-9515</issn><issn>1755-6724</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNqNjE1qAkEQRhtJQPNzh8o-Az1q95D1oIm7wLiXSlujHWa6THUn4AECyRU8i3fyCmnEA2T1PT4eb6BGZWVMYavx9Cqz1rp4MqUZqpsY37W2xpZmpL6fid2Weh-T7IFbqFHeOPiWhD8jNBjWMXGgCKfjT4OyRoE5S4_Jczgdfx9hhjEVNYUk2MFCML8HWPS7zruzBC0LvAp_UcDgCHIRluRy1DtoKCUfNnfqusUu0v1lb9XDfLasXwq35bD5yMZqJ75H2a-mk8racaUn_3H-ACrJVlc</recordid><startdate>2012</startdate><enddate>2012</enddate><creator>Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE</creator><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope></search><sort><creationdate>2012</creationdate><title>Geochemistry of Carboniferous Sandstones （Sardar Formation）, East-Central Iran： Implication for Provenance and Tectonic Setting</title><author>Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-chongqing_primary_437662703</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>伊朗</topic><topic>地球化学分析</topic><topic>地球化学特征</topic><topic>构造环境</topic><topic>物源</topic><topic>石炭纪</topic><topic>砂岩</topic><topic>被动大陆边缘</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><jtitle>地质学报：英文版</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mohammad KHANEHBAD Reza MOUSSAVI-HARAMI Asadollah MAHBOUBI Mehdi NADJAFI Mohammad Hosein MAHMUDY GHARAIE</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geochemistry of Carboniferous Sandstones （Sardar Formation）, East-Central Iran： Implication for Provenance and Tectonic Setting</atitle><jtitle>地质学报：英文版</jtitle><addtitle>Acta Geologica Sinica</addtitle><date>2012</date><risdate>2012</risdate><volume>86</volume><issue>5</issue><spage>1200</spage><epage>1210</epage><pages>1200-1210</pages><issn>1000-9515</issn><eissn>1755-6724</eissn><abstract>Geochemical analysis of sandstones from the Sardar Formation （from two stratigraphic successions） in east-central Iran were used for identification of geochemical characterization of sandstones, provenance and tectonic setting. Sandstones in the two lithostratigraphic successions have similar chemical compositions suggesting a common provenance. Bulk-rock geochemistry analysis of Carboniferous sandstones from Sardar Formation indicates that they are mainly quartz dominated and are classified as quartzarenites, sublitharenites and subarkoses, derived from acid igneous to intermediate igneous rocks. Discrimination function analysis indicates that the sandstones of Sardar Formation were derived from quartzose sedimentary provenance in a recycled orogenic setting. Also, major and trace elements in sandstones of Sardar Formation （e.g., K2O/Na2O vs. SiO2 ） indicate deposition in a stable passive continental margin （PM）. Chemical index of alteration （CIA） for these rocks （65%） suggests a moderate to relatively high degree of weathering in the source area.</abstract></addata></record>
fulltext fulltext
identifier ISSN: 1000-9515
ispartof 地质学报：英文版, 2012, Vol.86 (5), p.1200-1210
issn 1000-9515
1755-6724
language eng
recordid cdi_chongqing_primary_43766270
source Wiley-Blackwell Read & Publish Collection
subjects 伊朗
地球化学分析
地球化学特征
构造环境
物源
石炭纪
砂岩
被动大陆边缘
title Geochemistry of Carboniferous Sandstones （Sardar Formation）, East-Central Iran： Implication for Provenance and Tectonic Setting
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-02T07%3A42%3A55IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-chongqing&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Geochemistry%20of%20Carboniferous%20Sandstones%20%EF%BC%88Sardar%20Formation%EF%BC%89,%20East-Central%20Iran%EF%BC%9A%20Implication%20for%20Provenance%20and%20Tectonic%20Setting&rft.jtitle=%E5%9C%B0%E8%B4%A8%E5%AD%A6%E6%8A%A5%EF%BC%9A%E8%8B%B1%E6%96%87%E7%89%88&rft.au=Mohammad%20KHANEHBAD%20Reza%20MOUSSAVI-HARAMI%20Asadollah%20MAHBOUBI%20Mehdi%20NADJAFI%20Mohammad%20Hosein%20MAHMUDY%20GHARAIE&rft.date=2012&rft.volume=86&rft.issue=5&rft.spage=1200&rft.epage=1210&rft.pages=1200-1210&rft.issn=1000-9515&rft.eissn=1755-6724&rft_id=info:doi/&rft_dat=%3Cchongqing%3E43766270%3C/chongqing%3E%3Cgrp_id%3Ecdi_FETCH-chongqing_primary_437662703%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_id=info:pmid/&rft_cqvip_id=43766270&rfr_iscdi=true