Geology of the Ranger Uranium Mine, Northern Territory, Australia: structural constraints on the timing of uranium emplacement

摘要

The geology of the No 1 and 3 pits at the Ranger Mine in the Pine Creek Inlier (PCI) of Australia is dominated by Palaeoproterozoic volcanic, carbonate and sedimentary sequences that unconformably overlie Archaean granitic gneiss of the Nanambu Complex (2470 +- 50 Ma). These sequences are folded, faulted and sheared, and crosscut by east-trending granite (sensu stricto) dykes and pegmatite veins, and gently dipping N-NE trending mafic dykes of the Oenpelli Dolerite (approx 1690 Ma). Regional metamorphism is to greenschist facies and contact metamorphism is to hornblende-hornfels facies. The rocks of the Ranger Mine have been subjected to at least two phases of ductile-brittle deformation (D2-D3) and one phase of brittle deformation (D4). These events were preceded by regional diastathermal or extension-related metamorphism (D1) and the development of an ubiquitous bedding-parallel cleavage (S 1). D2 resulted in the development of NNE-NNW trending mesoscopic folds (F2) and a network of thrusts and dextral reverse shears. The modelled palaeo-stress directions for the emplacement of pegmatite veins suggests that they formed early in D2. D3 resulted in the development of WNW-NW trending mesoscopic folds (F3), a weakly defined axial planar cleavage (S3) and sinistral reactivation of D2 shears. D2-D3 are correlated with deformation during the Maud Creek Event of the Top End Orogeny (1870-1780 Ma), while the emplacement of granite dykes and pegmatite veins is correlated with emplacement of regional granites at 1870-1860 Ma. D4 is associated with brittle deformation and resulted in the development of normal faults and fault breccias during a period of east-west extension. This event is correlated with regional east-west extension during deposition of Palaeo- to Mesoproterozoic platform sequences. The sequence of tectonic events established in this study indicates that uranium-bearing ore shoots in the Ranger No 1 and 3 pits formed during extension in D4, and after emplacement of the Oenpelli Dolerite at 1690 Ma. However, the currently accepted 1737 +- 20 U-Pb Ma age places the mineralising event at time of regional post-orogenic erosion, after the Top End Orogeny and before emplacement of the Oenpelli Dolerite and extension in D4. The U-Pb age is not consistent with Sm-Nd ages for primary uranium mineralisation at Nabarlek and Jabiluka at 1650 Ma (Econ. Geol. 84 (1989) 64) and does not concur with currently accepted regional tectonic data of Johnston (Johnston, J.D., 1984. Structural evolution of the Pine Creek Inlier and mineralisation therein, Northern Territory, Australia. Unpublished PhD Thesis, Monash University, Australia), Needham et al. (Precambrian Res. 40/41(1988) 543) and others. Consequently, the absolute age of uranium mineralisation at the Ranger Mine is open.