The ‘pargasosphere’ hypothesis: Looking at global plate tectonics from a new perspective
نویسندگان
چکیده
Apart from the lithosphere-asthenosphere boundary (LAB), mid-lithospheric discontinuities (MLDs) in thick and old continental lithospheres appear to play an important role global plate tectonics. Initiation of intra-continental subduction, delamination lower lithospheric mantle removal cratonic roots are likely occur along MLDs. Here we introduce ‘pargasosphere’ hypothesis which could account for origin both boundaries. The observation that pargasitic amphibole is stable even at very low bulk ‘water’ concentration (~a few hundreds ppm wt.) implies solidus shallow upper (<3 GPa) usually pargasite dehydration ~1100 °C. In young oceanic lithosphere (<70 Ma) this defines LAB. LAB separates deeper, partial melt bearing asthenosphere shallower barren lithosphere, explaining their contrasting rheology. continents breaks down sub-solidus ~3 GPa liberates ‘water’-rich fluids. This latter process may be responsible formation occurrence melts or fluids beyond stability field can explain commonly observed geophysical anomalies associated with We present forward modelled variations shear wave velocity resistivity MLDs idealised columns. These columns constructed based on geotherms corresponding various tectono-thermal ages. offers a number other empirically testable implications. For instance, cooling beneath extensional settings source surface CO 2 emanations locations distant areas active volcanoes. Vrancea zone (Eastern Europe) appears suitable site testing elucidating intermediate-depth earthquakes (70–300 km) mantle. • ‘Pargasosphere’ refers part where stable. rheology (<100 controlled by pargasite. limit mid-lithosphere discontinuities. Along horizon, delaminate. asthenosphere, lead emission.
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ژورنال
عنوان ژورنال: Global and Planetary Change
سال: 2021
ISSN: ['0921-8181', '1872-6364']
DOI: https://doi.org/10.1016/j.gloplacha.2021.103547