福建紫金山矿田早白垩世以来构造演化和成岩成矿时空格架
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摘要
在充分吸收已有工作成果的基础上,文章系统总结了紫金山矿田的典型矿床类型及特征,探讨了早白垩世伸展构造背景下该矿田成岩成矿作用与北西向上杭—云霄成矿带的关系,并建立了早白垩世(145 Ma～)到晚白垩世早期(～92 Ma)紫金山矿田成岩成矿作用的时空格架。研究认为由于古太平洋板块俯冲作用体系的影响,早白垩世以来(145 Ma～)紫金山矿田总体上受北西向上杭—云霄深断裂多次活化作用的控制,依次经历了145～120 Ma伸展初期小规模的岩浆—成矿活动、125～110 Ma短暂的岩浆间歇期、110～92 Ma幔源物质大规模参与的岩浆活动及相应的斑岩型—浅成低温热液型(Cu-Au-Mo-Ag)多金属成矿作用。
This paper presents a systematic review of major types and characteristics of the representative deposits in the Zijinshan ore-field by integrating with previous studies,which is in an attempt to establish the spatial-temporal framework of magmatic-metallogenic events during 145 ～ 92 Ma time interval and,on that basis,investigate its relationship with the NW-trending Shanghang-Yunxiao mineralization belt under the Early Cretaceous extension setting. We conclude that the magmatism-mineraliztion of the Zijinshanore-field was mainly controlled by the multiple activation of the NW-trending Shanghang-Yunxiao deep fault in response to Pacific plate subduction. There occurred a small scale of the magmatism and metallogenesis in the Zijinshan ore-field when the regional tectonic regime inversed from compression to extension( 145 ～ 125 Ma),whereas the intense crust-mantle interaction induced large scale of magmatism and mineralization during the 110 ～ 92 Ma in response to the enhanced crust extension,which resulted in generating the giant Zijinshan porphyry-epithermal Cu-Au-Mo-Ag ore system. It's worth noting that a transient tectonic inversion lasted from 125 ～ 110 Ma separated the two extension stage mentioned above.These transpression gave rise to the short magmatic quiescence in our study area.
This paper presents a systematic review of major types and characteristics of the representative deposits in the Zijinshan ore-field by integrating with previous studies,which is in an attempt to establish the spatial-temporal framework of magmatic-metallogenic events during 145 ～ 92 Ma time interval and,on that basis,investigate its relationship with the NW-trending Shanghang-Yunxiao mineralization belt under the Early Cretaceous extension setting. We conclude that the magmatism-mineraliztion of the Zijinshanore-field was mainly controlled by the multiple activation of the NW-trending Shanghang-Yunxiao deep fault in response to Pacific plate subduction. There occurred a small scale of the magmatism and metallogenesis in the Zijinshan ore-field when the regional tectonic regime inversed from compression to extension( 145 ～ 125 Ma),whereas the intense crust-mantle interaction induced large scale of magmatism and mineralization during the 110 ～ 92 Ma in response to the enhanced crust extension,which resulted in generating the giant Zijinshan porphyry-epithermal Cu-Au-Mo-Ag ore system. It's worth noting that a transient tectonic inversion lasted from 125 ～ 110 Ma separated the two extension stage mentioned above.These transpression gave rise to the short magmatic quiescence in our study area.
引文
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