Geochemistry and Geochronology of the High-Mg Gabbro Dykes from Quanji Massif: Implications for the Amalgamation of Tarim Block in NW China and Assembly of the Rodinia Supercontinent

Geochemistry and Geochronology of the High-Mg Gabbro Dykes from Quanji Massif: Implications for the Amalgamation of Tarim Block in NW China and Assembly of the Rodinia Supercontinent

<正>The Tarim Craton is one of the major continental blocks in China.Mafic dykes,ultra-mafic–mafic–carbonatite complex and ultra-mafic–mafic pluton of 0.82–0.75 Ga widely occur in Kuluktage,Aksu and Tieklik area along

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Veröffentlicht in:Acta geologica Sinica (Beijing) 2016-10, Vol.90 (s1), p.104-105
Hauptverfasser: LIAO, Fanxi, CHEN, Nengsong, Santosh, M., SUN, Min, WANG, Qinyan, XU, Yixian
Format: Artikel
Sprache:eng
Schlagworte:
Amalgamation
Dikes
Gabbro
Geochemistry
Geochronology
Geochronometry
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Zusammenfassung:<正>The Tarim Craton is one of the major continental blocks in China.Mafic dykes,ultra-mafic–mafic–carbonatite complex and ultra-mafic–mafic pluton of 0.82–0.75 Ga widely occur in Kuluktage,Aksu and Tieklik area along
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.12913