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mantle flow that drives significant vertical motions of the crust along large areas(passive) is caused byMantle dynamic topography
the three distinct modes of slipcreateanisotropic dynamics
to address this problem , working with bodies of all shapes , ages , and sizes(passive) is designedReposturing dynamics
If ultralow velocity zones are hot and strongly enriched in iron , their exceptionally low thermal conductivity will delay their coolinginfluencinglowermost mantle dynamics
Tom Woodruff and Alec Gills , who worked with Hydraulx on AVP - R(passive) led byAmalgamated Dynamics
modulations of Vmax ... essentialto createhexose dynamics
an evolving grain sizewould influencemantle dynamics
plague(passive) have been ... influenced byspatiotemporal dynamics
the extent to whichinfluenceslower - mantle dynamics
not Jon Vagg wasto createthe read Mantle Dynamics
to further accumulation of this material into the ultralow - velocity patches that are observable by seismology.〈brmay leadto further accumulation of this material into the ultralow - velocity patches that are observable by seismology.〈br
in compositional and isotopic heterogeneity of the different mantle sectorsresultingin compositional and isotopic heterogeneity of the different mantle sectors
to the topographic development of orogensmay contributeto the topographic development of orogens
the deflections(passive) caused bythe deflections
near the large low shear velocity layers in the Pacific and Africaoriginatingnear the large low shear velocity layers in the Pacific and Africa
Miocene Amazon River drainage reversal(passive) caused byMiocene Amazon River drainage reversal
epeirogenic transients(passive) caused byepeirogenic transients
the syn-do ... influencethe syn-