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Article: Petrochemistry and mineral chemistry studies on metamorphic ultramafic rocks in Yanghou area, Zhenghe Country, Fujian Province, China

TitlePetrochemistry and mineral chemistry studies on metamorphic ultramafic rocks in Yanghou area, Zhenghe Country, Fujian Province, China
闽北政和洋后变质超镁铁岩的岩石地球化学及矿物化学研究
Authors
Keywords岩石地球化学 (Lithogeochemistry)
矿物化学 (Mineral chemistry)
年代學 (Chronology)
变质超镁铁岩 (Metamorphic ultramafic)
福建省 (Fujian Province)
Issue Date1997
PublisherKe xue chu ban she.
Citation
Geochimica, 1997, v. 26 n. 4, p. 13-23 How to Cite?
地球化学, 1997, 第26卷 第4期, pp. 13-23 How to Cite?
AbstractPetrochemistry studies indicate that the Yanghou metamorphic ultramafic rocksare composed of metamorphosed harzburgite and burgite and ultramafic cumulate . Trace element geochemistry and mineral chemistry studies on the metamorphosed harzburgite indicate that it is the relict of the depleted mantle. From systematic studies on petrochemistry , mineral chemistry and geochronology, it s concluded that the Yanghou metamorphic ultramafic rocks are components of Later Sinian-Early Paleozoic ophiolite in South China.
岩石化学研究表明, 洋后变质超镁铁岩是由变质方辉橄榄岩和变质超镁铁堆积岩组成。变质方辉橄榄岩的微量元素地球化学及矿物化学特征表明, 应为亏损的残余地慢产物。通过系统的岩石地球化学、矿物化学及年代学研究, 认为洋后变质超镁铁岩可能为华南晚震旦一早古生代的蛇绿岩组成部分。
Persistent Identifierhttp://hdl.handle.net/10722/73061
ISSN

 

DC FieldValueLanguage
dc.contributor.authorRen, SLen_HK
dc.contributor.authorLi, JLen_HK
dc.contributor.authorZhou, XHen_HK
dc.contributor.authorSun, Men_HK
dc.date.accessioned2010-09-06T06:47:41Z-
dc.date.available2010-09-06T06:47:41Z-
dc.date.issued1997en_HK
dc.identifier.citationGeochimica, 1997, v. 26 n. 4, p. 13-23en_HK
dc.identifier.citation地球化学, 1997, 第26卷 第4期, pp. 13-23-
dc.identifier.issn0379-1726en_HK
dc.identifier.urihttp://hdl.handle.net/10722/73061-
dc.description.abstractPetrochemistry studies indicate that the Yanghou metamorphic ultramafic rocksare composed of metamorphosed harzburgite and burgite and ultramafic cumulate . Trace element geochemistry and mineral chemistry studies on the metamorphosed harzburgite indicate that it is the relict of the depleted mantle. From systematic studies on petrochemistry , mineral chemistry and geochronology, it s concluded that the Yanghou metamorphic ultramafic rocks are components of Later Sinian-Early Paleozoic ophiolite in South China.-
dc.description.abstract岩石化学研究表明, 洋后变质超镁铁岩是由变质方辉橄榄岩和变质超镁铁堆积岩组成。变质方辉橄榄岩的微量元素地球化学及矿物化学特征表明, 应为亏损的残余地慢产物。通过系统的岩石地球化学、矿物化学及年代学研究, 认为洋后变质超镁铁岩可能为华南晚震旦一早古生代的蛇绿岩组成部分。-
dc.languagechien_HK
dc.publisherKe xue chu ban she.en_HK
dc.relation.ispartofGeochimicaen_HK
dc.relation.ispartof地球化学-
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License-
dc.subject岩石地球化学 (Lithogeochemistry)-
dc.subject矿物化学 (Mineral chemistry)-
dc.subject年代學 (Chronology)-
dc.subject变质超镁铁岩 (Metamorphic ultramafic)-
dc.subject福建省 (Fujian Province)-
dc.titlePetrochemistry and mineral chemistry studies on metamorphic ultramafic rocks in Yanghou area, Zhenghe Country, Fujian Province, Chinaen_HK
dc.title闽北政和洋后变质超镁铁岩的岩石地球化学及矿物化学研究-
dc.typeArticleen_HK
dc.identifier.emailSun, M: minsun@hku.hken_HK
dc.identifier.authoritySun, M=rp00780en_HK
dc.description.naturepublished_or_final_version-
dc.identifier.hkuros34280en_HK
dc.identifier.volume26-
dc.identifier.issue4-
dc.identifier.spage13-
dc.identifier.epage23-
dc.publisher.placeChina-

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