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The Olympic Cu-Au Province, Gawler Craton: A Review of the Lithospheric Architecture, Geodynamic Setting, Alteration Systems, Cover Successions and Prospectivity

机译:奥林匹克古奥省,高勒·克拉顿:岩石圈建筑学,地球动力学背景,蚀变系统,覆盖演替和展望的回顾

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The Olympic Cu-Au Province is a metallogenic province in South Australia that contains one of the world’s most significant Cu-Au-U resources in the Olympic Dam deposit. The Olympic Cu-Au Province also hosts a range of other iron oxide-copper-gold (IOCG) deposits including Prominent Hill and Carrapateena. This paper reviews the geology of the Olympic Cu-Au Province by investigating the lithospheric architecture, geodynamic setting and alteration systematics. In addition, since the province is almost entirely buried by post-mineral cover, the sedimentary cover sequences are also reviewed. The Olympic Cu-Au Province formed during the early Mesoproterozoic, ca. 1.6 Ga and is co-located with a fundamental lithospheric boundary in the eastern Gawler Craton. This metallogenic event was driven in part by melting of a fertile, metasomatized sub-continental lithospheric mantle during a major regional tectonothermal event. Fluid evolution and multiple fluid mixing resulted in alteration assemblages that range from albite, magnetite and other higher temperature minerals to lower temperature assemblages such as hematite, sericite and chlorite. IOCG mineralisation is associated with both high and low temperature assemblages, however, hematite-rich IOCGs are the most economically significant. Burial by Mesoproterzoic and Neoproterozoic-Cambrian sedimentary successions preserved the Olympic Cu-Au Province from erosion, while also providing a challenge for mineral exploration in the region. Mineral potential modelling identifies regions within the Olympic Cu-Au Province and adjacent Curnamona Province that have high prospects for future IOCG discoveries. Exploration success will rely on improvements in existing potential field and geochemical data, and be bolstered by new 3D magnetotelluric surveys. However, drilling remains the final method for discovery of new mineral resources.
机译:奥林匹克铜金省是南澳大利亚州的一个成矿省,奥林匹克水坝矿床中蕴藏着世界上最重要的铜金铀资源之一。奥林匹克古奥省还拥有一系列其他的氧化铁-铜-金(IOCG)矿床,包括Prominent Hill和Carrapateena。本文通过研究岩石圈的建筑,地球动力环境和蚀变系统,回顾了奥林匹克古奥省的地质情况。此外,由于该省几乎完全被矿产后的掩埋物掩埋,因此还对沉积物的掩盖顺序进行了审查。奥林匹克古奥省在中元古代早期形成。 1.6 Ga并与Gawler Craton东部的岩石圈基本边界共存。该成矿事件的部分原因是在一次主要的区域构造热事件中,一块肥沃的,交代了的亚大陆岩石圈地幔融化了。流体的演化和多种流体的混合导致了变化的组合,从钠长石,磁铁矿和其他高温矿物到低温组合,例如赤铁矿,绢云母和绿泥石。 IOCG矿化与高温和低温组合都有关,但是,富含赤铁矿的IOCG具有最经济的意义。中元古代和新元古代-寒武纪沉积演习的埋葬使奥林匹克古奥省免受侵蚀,同时也对该地区的矿物勘探带来了挑战。矿物势模型确定了奥林匹克古奥省和库纳莫纳省附近的地区,这些地区对于未来的IOCG发现具有很高的前景。勘探成功将取决于对现有潜在油田和地球化学数据的改进,并受到新的3D大地电磁勘探的支持。但是,钻探仍然是发现新矿产资源的最终方法。

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