Metallogenic age and genesis of Jinshan gold deposit, Jiangxi Province, China
Identifieur interne : 001943 ( Main/Exploration ); précédent : 001942; suivant : 001944Metallogenic age and genesis of Jinshan gold deposit, Jiangxi Province, China
Auteurs : Xiuzhang Wang [République populaire de Chine] ; Qiang Shan [République populaire de Chine] ; Huaying Liang [République populaire de Chine] ; Jingping Cheng [République populaire de Chine] ; Ping Xia [République populaire de Chine]Source :
- Chinese Journal of Geochemistry [ 1000-9426 ] ; 2000-06-01.
English descriptors
- KwdEn :
Abstract
Abstract: The Jinshan gold deposit consists of gold-bearing ultramylonite and gold-bearing quartz vein ores. The Rb-Sr isochron age of fluid inclusions in quartz from quartz veins is the same as that of the gold-bearing ultramylonite, suggesting that both the types of orebodies were formed simultaneously in the Caledonian period, in the range 406–409 Ma. REE patterns and sulfur, lead, carbon, hydrogen and oxygen isotope data, as well as the composition of fluid inclusions, have shown that the ore-forming fluids were derived from formation water, and the ore-forming materials came from the gold-hosted rocks. The Jinshan gold deposit occurring in a Caledonian brittle-ductile zone in metamorphosed microclastic rocks owes its origin to Caledonian reworking processes.
Url:
DOI: 10.1007/BF03166864
Affiliations:
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J. of Geochem.</title><idno type="ISSN">1000-9426</idno><idno type="eISSN">1993-0364</idno><imprint><publisher>Science in China Press</publisher><pubPlace>Beijing</pubPlace><date type="published" when="2000-06-01">2000-06-01</date><biblScope unit="volume">19</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="97">97</biblScope><biblScope unit="page" to="104">104</biblScope></imprint><idno type="ISSN">1000-9426</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1000-9426</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Caledonian period</term><term>Jinshan gold deposit</term><term>gold-bearing quartz vein</term><term>gold-bearing siliceous ultramylonite</term><term>reworking genesis</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: The Jinshan gold deposit consists of gold-bearing ultramylonite and gold-bearing quartz vein ores. The Rb-Sr isochron age of fluid inclusions in quartz from quartz veins is the same as that of the gold-bearing ultramylonite, suggesting that both the types of orebodies were formed simultaneously in the Caledonian period, in the range 406–409 Ma. REE patterns and sulfur, lead, carbon, hydrogen and oxygen isotope data, as well as the composition of fluid inclusions, have shown that the ore-forming fluids were derived from formation water, and the ore-forming materials came from the gold-hosted rocks. The Jinshan gold deposit occurring in a Caledonian brittle-ductile zone in metamorphosed microclastic rocks owes its origin to Caledonian reworking processes.</div></front></TEI><affiliations><list><country><li>République populaire de Chine</li></country><region><li>Guangdong</li></region><settlement><li>Jiangmen</li></settlement></list><tree><country name="République populaire de Chine"><region name="Guangdong"><name sortKey="Wang, Xiuzhang" sort="Wang, Xiuzhang" uniqKey="Wang X" first="Xiuzhang" last="Wang">Xiuzhang Wang</name></region><name sortKey="Cheng, Jingping" sort="Cheng, Jingping" uniqKey="Cheng J" first="Jingping" last="Cheng">Jingping Cheng</name><name sortKey="Liang, Huaying" sort="Liang, Huaying" uniqKey="Liang H" first="Huaying" last="Liang">Huaying Liang</name><name sortKey="Shan, Qiang" sort="Shan, Qiang" uniqKey="Shan Q" first="Qiang" last="Shan">Qiang Shan</name><name sortKey="Xia, Ping" sort="Xia, Ping" uniqKey="Xia P" first="Ping" last="Xia">Ping Xia</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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