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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
intracontinental belts
Development of an intracontinental plate boundary transfer zone, Marlborough, Aotearoa New Zealand: A review and synthesis Available to Purchase
Porphyry Mo mineralization related to adakite-like magmas in an intra-continental extensional setting at the Aolunhua deposit, northeastern China Available to Purchase
The early Paleozoic intracontinental orogeny in South China: A far-field response to the closure of the Proto-Tethys Ocean in the Indochina Block Available to Purchase
Insights into the Phanerozoic evolution of the São Francisco Craton based on detrital zircon thermochronology and U-Pb-Hf geochronology Available to Purchase
Impact of rift history on the structural style of intracontinental rift-inversion orogens Open Access
The production of parallel world-class W and Cu metallogenic belts linked to an asymmetric slab window Available to Purchase
Geophysical constraints on continental rejuvenation in central China: Implications for outward growth of the Tibetan Plateau Available to Purchase
Cenozoic dextral transpressional tectonics in the northwestern Qaidam Basin, northern Tibet: Evidence from paleomagnetic and kinematic analysis of the arcuate belts Available to Purchase
High-resolution chronostratigraphy of late Mesozoic sequences in northern North China: Implications for the linkages among intracontinental orogeny, volcanism, Jehol Biota, and Pacific plate subduction Available to Purchase
Extent and significance of the Racklan–Forward Orogen in Canada: far-field interior reactivation during Nuna assembly Available to Purchase
Abstract Mesoproterozoic orogenesis is well established on the western and southern flanks of Laurentia in the well-known Racklan–Forward and Mazatzal orogens, but its significance within the previously assembled interior of the supercontinent Nuna has not been established. We examine regional isotopic and structural evidence for Mesoproterozoic deformation in the c. 1.7–1.63 Ga Hornby Bay, Elu, Thelon and Athabasca intracontinental basins, and present evidence for Mesoproterozoic reactivation of Paleoproterozoic structures in the Wopmay and Trans-Hudson orogens. The Racklan–Forward Orogeny in the interior of north Laurentia comprises north–south-trending, high-angle, east-vergent folds and thrusts that occur across a region 1660 km wide and over 1000 km long, stretching from the Yukon to near Hudson Bay and from Banks Island to below the Western Canada Sedimentary Basin. The structures progress from ductile amphibolite and greenschist facies in the Racklan type area to sub-greenschist facies and ultimately brittle or brittle-ductile in the far foreland, showing a predominant thick-skinned style typical of many intracontinental orogens. We present compiled low-temperature thermochronological data, including ages of spatially associated uraninite mineralization, to characterize the scope of reactivation of basement structures in the Archean Rae craton in Nuna's interior. We compare the nature of widespread far-field reactivation in the Racklan–Forward Orogen with other orogens of Nuna's assembly to show it is unusual for Nuna's peripheral margin. We suggest that c. 1.6 Ga continent–continent collision of North Australia with NW Laurentia propagated stresses far into the interior as a result of combined favourable pre-existing structural grain and a weak subcontinental lithospheric mantle in the Rae craton due to repeated episodes of refertilization across 500 Ma of accretion and intrusion. Cratons that experience the complex, two-sided collision and protracted upper plate setting during supercontinent assembly noted herein may be particularly susceptible to extensive foreland propagation of peripheral orogens.