Metamorphic T/P ratios and corresponding geothermal gradients for high-grade metamorphic rocks from both Proto-Tethys and Paleo-Tethys tectonic domains shows an increasing trend with age. It appears that these high-grade metamorphic rocks experienced three types of regional metamorphism in terms of their metamorphic T/P ratios: (1) an early stage of low T/P Alpine-type blueschist- to eclogite-facies high-P to ultrahigh-P metamorphism; (2) a middle stage of medium T/P Barrovian-type medium-P amphibolite to high-P granulite-facies metamorphism; and (3) a late stage of the high T/P Buchan-type low P amphibolite to MP granulite-facies metamorphism. For the ages of Alpine-type, Barrovian-type, and Buchan-type metamorphisms, they occurred at 500 to 400 Ma in the Paleozoic for the Proto-Tethys tectonic domain and 250 to 120 Ma in the Mesozoic for the Paleo-Tethys tectonic domain.
Convergent continental margins are characterized by the change of geothermal gradients during their tectonic evolution from dynamic compression to extension, giving rise to metamorphic rocks with different T/P ratios. In the stage of oceanic subduction, low geothermal gradients make cold subduction to produces low T/P Alpine-type metamorphic rocks. In the continental subduction/collision stage, the deep subduction of continental crust took place at low geothermal gradients but its collisional thickening occurred at moderate geothermal gradients. Therefore, this stage would produce both low T/P Alpine-type and moderate T/P Barrovian-type metamorphic rocks. In the post-collisional stage, the thickened continental lithosphere was thinned due to its gravitational or rheological instability, inducing asthenospheric upwelling and leading the thinned lithosphere to high geothermal gradients for high T/P Buchan-type metamorphism.
Based on the P-T information on and spatiotemporal relationships between the metamorphic rocks in the different orogens along the CCOS, the tectonic evolution of the Proto-Tethys and Paleo-Tethys tectonic domains can be reconstructed as follows. The continental collision/subduction in the Proto-Tethys orogenic system would occur either at 500-490 Ma in the Altyn, North Qinling and North Tongbai orogens, or at 450-430 Ma in the North Qaidam and East Kunlun orogens, and continental rifting would occur either at 460-450 Ma in the Altyn, North Qinling and North Tongbai orogens or at 410-400 Ma in the North Qaidam and East Kunlun orogens. On the other hand, continental subduction/collision in the Paleo-Tethys orogenic system would occur at 250-220 Ma, and continental rifting would occur at 140-120 Ma.
Although timescales of either continental deep subduction or hard collision are restricted to 10-30 Myr, time intervals between the low T/P Alpine-type metamorphism and the high T/P Buchan-type metamorphism are as short as about 40-60 Myr for the Proto-Tethys tectonic domain but as long as about 110 Myr for the Paleo-Tethys tectonic domain. These similarities and differences indicate that the high-grade metamorphic rocks in the two different Tethys tectonic domains record the tectonic transition of convergent continental margins from cold subduction through warm collision or exhumation to hot rifting. This is associated with the metamorphic transformation from the early Alpine-type facies series to the late Barrovian-type facies series, and then superimposition by Buchan-type facies series.
Research Report:The influence of Tethyan evolution on changes of the Earth's past environment
Research Report:Metamorphic evolution of the East Tethys tectonic domain and its tectonic implications
Related Links
University of Science and Technology of China
Tectonic Science and News
| Subscribe Free To Our Daily Newsletters |
| Subscribe Free To Our Daily Newsletters |
