Record of mid-Archaean subduction from metamorphism in the Barberton terrain, South Africa
dc.contributor.author | Moyen J.-F. | |
dc.contributor.author | Stevens G. | |
dc.contributor.author | Kisters A. | |
dc.date.accessioned | 2011-05-15T16:02:07Z | |
dc.date.available | 2011-05-15T16:02:07Z | |
dc.date.issued | 2006 | |
dc.description.abstract | Although plate tectonics is the central geological process of the modern Earth, its form and existence during the Archaean era (4.0-2.5 Gyr ago) are disputed. The existence of subduction during this time is particularly controversial because characteristic subduction-related mineral assemblages, typically documenting apparent geothermal gradients of 15°C km-1 or less, have not yet been recorded from in situ Archaean rocks (the lowest recorded apparent geothermal gradients are greater than 25°C km -1). Despite this absence from the rock record, low Archaean geothermal gradients are suggested by eclogitic nodules in kimberlites and circumstantial evidence for subduction processes, including possible accretion-related structures, has been reported in Archaean terrains. The lack of spatially and temporally well-constrained high-pressure, low-temperature metamorphism continues, however, to cast doubt on the relevance of subduction-driven tectonics during the first 1.5 Gyr of the Earth's history. Here we report garnet-albite-bearing mineral assemblages that record pressures of 1.2-1.5 GPa at temperatures of 600-650°C from supracrustal amphibolites from the mid-Archaean Barberton granitoid-greenstone terrain. These conditions point to apparent geothermal gradients of 12-15°C-similar to those found in recent subduction zones-that coincided with the main phase of terrane accretion in the structurally overlying Barberton greenstone belt. These high-pressure, low-temperature conditions represent metamorphic evidence for cold and strong lithosphere, as well as subduction-driven tectonic processes, during the evolution of the early Earth. © 2006 Nature Publishing Group. | |
dc.description.version | Article | |
dc.identifier.citation | Nature | |
dc.identifier.citation | 442 | |
dc.identifier.citation | 7102 | |
dc.identifier.issn | 280836 | |
dc.identifier.other | 10.1038/nature04972 | |
dc.identifier.uri | http://hdl.handle.net/10019.1/12320 | |
dc.subject | Geology | |
dc.subject | Geothermal energy | |
dc.subject | High pressure effects | |
dc.subject | Low temperature effects | |
dc.subject | Mineral resources | |
dc.subject | Rocks | |
dc.subject | Geological processes | |
dc.subject | Geothermal gradients | |
dc.subject | Metamorphism | |
dc.subject | Subduction | |
dc.subject | Supracrustal amphibolites | |
dc.subject | Tectonics | |
dc.subject | amphibole | |
dc.subject | Archean | |
dc.subject | geothermal gradient | |
dc.subject | kimberlite | |
dc.subject | metamorphism | |
dc.subject | plate tectonics | |
dc.subject | subduction | |
dc.subject | article | |
dc.subject | evolution | |
dc.subject | geographic and geological phenomena | |
dc.subject | geological time | |
dc.subject | low temperature | |
dc.subject | metamorphosis | |
dc.subject | priority journal | |
dc.subject | South Africa | |
dc.subject | Africa | |
dc.subject | Barberton | |
dc.subject | Mpumalanga | |
dc.subject | South Africa | |
dc.subject | Southern Africa | |
dc.subject | Sub-Saharan Africa | |
dc.title | Record of mid-Archaean subduction from metamorphism in the Barberton terrain, South Africa | |
dc.type | Article |