Geochemical and ion-microprobe U–Pb zircon constraints on the Archaean evolution of Singhbhum Craton, eastern India

Abstract

Geochemical and SHRIMP U–Pb zircon analyses were obtained for nine samples of the Singhbhum Craton to investigate major regional granite intrusion, volcanism, sedimentary deposition, metamorphism and deformation episodes. Detrital zircons within a recrystallized sandstone enclave within tonalitic gneiss provided a maximum time for deposition of 3375±3Ma (all uncertainties are at 95% confidence unless otherwise specified) for the host sandstone. Igneous crystallization dates between 3380 and 3299Ma were obtained for tonalite gneiss and foliated trondhjemite samples from widely dispersed sites, whereas unfoliated granitic samples provided igneous crystallization dates <3.3Ga, thus constraining the time of regional deformation and amphibolite grade metamorphism to the interval c. 3325–3300Ma. Volcanic, clastic sedimentary and banded iron-formation rocks assigned to the Iron Ore Group (IOG) are preserved around the margins of the Singhbhum Granite Complex. An igneous crystallization date of 3285±7Ma, obtained for a biotite granodiorite that is overlain by conglomerate of the IOG, provides a maximum deposition age for components within the western (Jamda-Koira) IOG basin. A dacite tuff from the Malayagiri IOG basin south of Palalahara yielded an igneous crystallization date of 2806±6Ma, confirming that the IOG as currently defined, includes unrelated sedimentary rocks that were deposited within different basins over an 800 Myr interval. Evolution of the Singhbhum Craton may be summarized as follows: (1) between 3530 and 3300Ma, tonalites were emplaced, with volcanic, clastic and carbonate rocks and banded iron-formation (cycle 1) deposited onto tonalitic basement until 3375Ma; (2) between 3325 and 3300Ma, burial, deformation and uplift transformed the central part of the Singhbhum basement to tonalite gneisses, with cycle 1 sedimentary rocks incorporated into the gneisses as enclaves but preserved within synforms around the basement margins; post-3.3Ga regional metamorphism granodiorite intrusions were emplaced until c. 3285Ma; (3) BIF and clastic sedimentary rocks (cycle 2) were deposited around the margins of the craton onto the older (cycle 1) sedimentary rocks and adjacent gneissic basement until c. 3.1Ga; (4) a further episode of granite intrusion at 3090Ma was followed by uplift and erosion of the central part of the craton prior to 2806Ma; (5) volcano-sedimentary and banded iron-formation rocks were deposited during a third sedimentary cycle at c. 2.8Ga.