AGE AND SOURCE MATERIALS OF BAJIATAN AND FANSHAN-SHIMATAN INTRUSIVE ROCKS IN LUJIANG-ZONGYANG DISTRICT, ANHUI PROVINCE
The Mesozoic volcanic rocks in Lujiang-Zongyang district can be divided into four formations, from early to late, Longmenyuan, Zhuanqiao, Shuangmiao, Fushan. Their isotopic ages are in confusion. For example, the 11 dating data of Zhuanqiao Formation are between 135 Ma and 109 Ma, belonging to K1, w...
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Veröffentlicht in: | 中国科学通报:英文版 1991 (19), p.1626-1628 |
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creator | 任启江 王德滋 刘孝善 杨荣勇 孙冶东 邱检生 |
description | The Mesozoic volcanic rocks in Lujiang-Zongyang district can be divided into four formations, from early to late, Longmenyuan, Zhuanqiao, Shuangmiao, Fushan. Their isotopic ages are in confusion. For example, the 11 dating data of Zhuanqiao Formation are between 135 Ma and 109 Ma, belonging to K1, whereas other 9 dating data are from 136 Ma to 178 Ma, belonging to J2—J3. Through the studies on Sm-Nd and Rb-Sr isotopic composition of the Bajiatan and Fanshan-Shimatan volcanic-intrusive rocks in the district, some significant data with regard to the ages and source materials of the volcanic-intrusive rocks have been acquired and published in this note. |
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Their isotopic ages are in confusion. For example, the 11 dating data of Zhuanqiao Formation are between 135 Ma and 109 Ma, belonging to K1, whereas other 9 dating data are from 136 Ma to 178 Ma, belonging to J2—J3. Through the studies on Sm-Nd and Rb-Sr isotopic composition of the Bajiatan and Fanshan-Shimatan volcanic-intrusive rocks in the district, some significant data with regard to the ages and source materials of the volcanic-intrusive rocks have been acquired and published in this note.</description><identifier>ISSN: 2095-9273</identifier><language>eng</language><subject>composition ; intrusive ; isotopic ; rocks ; volcanic</subject><ispartof>中国科学通报:英文版, 1991 (19), p.1626-1628</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/86894X/86894X.jpg</thumbnail><link.rule.ids>314,780,784,4022</link.rule.ids></links><search><creatorcontrib>任启江 王德滋 刘孝善 杨荣勇 孙冶东 邱检生</creatorcontrib><title>AGE AND SOURCE MATERIALS OF BAJIATAN AND FANSHAN-SHIMATAN INTRUSIVE ROCKS IN LUJIANG-ZONGYANG DISTRICT, ANHUI PROVINCE</title><title>中国科学通报:英文版</title><addtitle>Chinese Science Bulletin</addtitle><description>The Mesozoic volcanic rocks in Lujiang-Zongyang district can be divided into four formations, from early to late, Longmenyuan, Zhuanqiao, Shuangmiao, Fushan. 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Through the studies on Sm-Nd and Rb-Sr isotopic composition of the Bajiatan and Fanshan-Shimatan volcanic-intrusive rocks in the district, some significant data with regard to the ages and source materials of the volcanic-intrusive rocks have been acquired and published in this note.</description><subject>composition</subject><subject>intrusive</subject><subject>isotopic</subject><subject>rocks</subject><subject>volcanic</subject><issn>2095-9273</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1991</creationdate><recordtype>article</recordtype><recordid>eNqNTskKwjAUzEFBUf_hgVcLsSq1x2dM2-eSSJIKehERV9wLgn9vED_A0yzMDFNi1ZDHvSAOo06FNYrixDlvd-Owy6Mqe2EqAdUQrM6NkDBFJw3hxIJOYIAjQofqG0hQ2QxVYDOafk1SzuSW5hKMFmPrNUxyX1BpsNQqXXgCQ7LOkHAtP5HlBDOj56SErLPybn0uto0f1lgzkU5kweZwu-4fx-t-dX8eL-vne9XmvBf2-5G__1_qA6sGQOE</recordid><startdate>1991</startdate><enddate>1991</enddate><creator>任启江 王德滋 刘孝善 杨荣勇 孙冶东 邱检生</creator><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope></search><sort><creationdate>1991</creationdate><title>AGE AND SOURCE MATERIALS OF BAJIATAN AND FANSHAN-SHIMATAN INTRUSIVE ROCKS IN LUJIANG-ZONGYANG DISTRICT, ANHUI PROVINCE</title><author>任启江 王德滋 刘孝善 杨荣勇 孙冶东 邱检生</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-chongqing_primary_10052887273</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1991</creationdate><topic>composition</topic><topic>intrusive</topic><topic>isotopic</topic><topic>rocks</topic><topic>volcanic</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>任启江 王德滋 刘孝善 杨荣勇 孙冶东 邱检生</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- 镜像站点</collection><jtitle>中国科学通报:英文版</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>任启江 王德滋 刘孝善 杨荣勇 孙冶东 邱检生</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>AGE AND SOURCE MATERIALS OF BAJIATAN AND FANSHAN-SHIMATAN INTRUSIVE ROCKS IN LUJIANG-ZONGYANG DISTRICT, ANHUI PROVINCE</atitle><jtitle>中国科学通报:英文版</jtitle><addtitle>Chinese Science Bulletin</addtitle><date>1991</date><risdate>1991</risdate><issue>19</issue><spage>1626</spage><epage>1628</epage><pages>1626-1628</pages><issn>2095-9273</issn><abstract>The Mesozoic volcanic rocks in Lujiang-Zongyang district can be divided into four formations, from early to late, Longmenyuan, Zhuanqiao, Shuangmiao, Fushan. Their isotopic ages are in confusion. For example, the 11 dating data of Zhuanqiao Formation are between 135 Ma and 109 Ma, belonging to K1, whereas other 9 dating data are from 136 Ma to 178 Ma, belonging to J2—J3. Through the studies on Sm-Nd and Rb-Sr isotopic composition of the Bajiatan and Fanshan-Shimatan volcanic-intrusive rocks in the district, some significant data with regard to the ages and source materials of the volcanic-intrusive rocks have been acquired and published in this note.</abstract></addata></record> |
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issn | 2095-9273 |
language | eng |
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source | Alma/SFX Local Collection |
subjects | composition intrusive isotopic rocks volcanic |
title | AGE AND SOURCE MATERIALS OF BAJIATAN AND FANSHAN-SHIMATAN INTRUSIVE ROCKS IN LUJIANG-ZONGYANG DISTRICT, ANHUI PROVINCE |
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