Time scales and mechanisms of growth of active margins of Gondwana: A model based on detrital zircon ages from the Neoproterozoic to Cambrian Blovice accretionary complex, Bohemian Massif

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• 作者：Jaroslava Hajná ; ^a ; ^{jaruska@cbcnet.cz} ; Jiří ; Žá ; k^a ; Wolfgang Dö ; rr^b
• 关键词：Accretionary wedge ; Bohemian Massif ; U&ndash ; Pb geochronology ; Detrital zircons ; Cadomian orogeny
• 刊名：Gondwana Research
• 出版年：2017
• 出版时间：February 2017
• 年：2017
• 卷：42
• 期：Complete
• 页码：63-83
• 全文大小：7815 K
• 卷排序：42

文摘

Cadomian accretion in the Blovice accretionary complex lasted till ca. 527 Ma. Sedimentation in younger forearc basins continued at least till 499 Ma. Cadomian evolution of this complex is similar with that of the Ossa Morena.