Role of the transition zone and 660 km discontinuity in mantle dynamics

scientific article

Role of the transition zone and 660 km discontinuity in mantle dynamics is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode1994PEPI...86....5R
P356DOI10.1016/0031-9201(94)05058-9

P2093author name stringA.E. Ringwood
P433issue1-3
P304page(s)5-24
P577publication date1994-10-01
P1433published inPhysics of the Earth and Planetary InteriorsQ7189702
P1476titleRole of the transition zone and 660 km discontinuity in mantle dynamics
P478volume86

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cites work (P2860)
Q60722467Absence of density crossover between basalt and peridotite in the cold slabs passing through 660 km discontinuity
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Q107269633Garnet–ilmenite–perovskite transitions in the system Mg4Si4O12–Mg3Al2Si3O12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structure
Q60722222Influence of Water on Major Phase Transitions in the Earth's Mantle
Q60722502Mechanisms and kinetics of the post-spinel transformation in Mg2SiO4
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Q29396953The composition of the Earth
Q59056423The fate of subducted basaltic crust in the Earth's lower mantle
Q107275344Upper-mantle seismic discontinuities in a subduction zone (Japan) investigated from P to S converted waves

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