CO2 degassing and melting of metasomatized mantle lithosphere during rifting-Numerical study  

作　　者：Weronika Gorczyk Christopher M. Gonzalez 

机构地区：[1]University of Western Australia,Centre for Exploration Targeting,School of Earth Sciences,ARC Centre of Excellence for Core to Crust Fluid Systems,Perth,Western Australia,Australia [2]School of Earth,Atmosphere and Environment,Monash University Clayton,Melbourne,VIC,Australia

出　　处：《Geoscience Frontiers》2019年第4期1409-1420,共12页地学前缘（英文版）

基　　金：sponsored by ARC Centre of Excellence for Core toCrust Fluid Systems;provided by the Pawsey Supercomputing Centre with funding from the Australian Government and the Government of Western Australia

摘　　要：:Reactivation of metasomatized mantle lithosphere may occur during continental extension,which is an important component of plate tectonics.The lower most part of the metasomatized domains in the subcontinental mantle lithosphere can be locally enriched in CO2.Therefore,partial melting of these metasomatized domains may play a crucial role in the global carbon cycle.However,little is known about this process and up until now few numerical constraints are available.Here we address this knowledge gap and use a 2-D high resolution petrological-thermomechanical model to assess lithospheric rifting.CO2 degassing and melting.We test 4 lithospheric thicknesses:90,110,130 and 200 km with a 10 km thick metasomatized layer at the base using CO2 of 2 wt.%in the bulk composition.The carbonate enriched layer is stable below^3 GPa(>110 km)for a temperature of 1300℃;therefore,we only observe degassing patterns for lithospheric models that are 130 km and 200 km thick.The metasomatized layer for the 130 km thick lithosphere mostly comprises carbonatite melting,whereas in the 200 km thick scenario propagation of melt development from kimberlites to carbonatites occurs as the metasomatic mantle is exhumed during extension.The numerical models fit well into natural rifting zones of the European Cenozoic Rift System for young(shallow)and of the North Atlantic Rift for old(thick)lithosphere.Reactivation of metasomatized mantle lithosphere may occur during continental extension,which is an important component of plate tectonics.The lower most part of the metasomatized domains in the subcontinental mantle lithosphere can be locally enriched in CO2.Therefore,partial melting of these metasomatized domains may play a crucial role in the global carbon cycle.However,little is known about this process and up until now few numerical constraints are available.Here we address this knowledge gap and use a 2-D high resolution petrological-thermomechanical model to assess lithospheric rifting.CO2 degassing and melting.We test 4 lithospheric thicknesses:90,110,130 and 200 km with a 10 km thick metasomatized layer at the base using CO2 of 2 wt.% in the bulk composition.The carbonate enriched layer is stable below ～3 GPa（>110 km）for a temperature of 1300 ℃; therefore,we only observe degassing patterns for lithospheric models that are 130 km and 200 km thick.The metasomatized layer for the 130 km thick lithosphere mostly comprises carbonatite melting,whereas in the200 km thick scenario propagation of melt development from kimberlites to carbonatites occurs as the metasomatic mantle is exhumed during extension.The numerical models fit well into natural rifting zones of the European Cenozoic Rift System for young（shallow）and of the North Atlantic Rift for old（thick）lithosphere.

关 键 词：RIFTING MANTLE CO2 DEGASSING CARBONATE MELTING 

分 类 号：P[天文地球]