| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2000JGR...10516359P |
| P356 | DOI | 10.1029/2000JB900080 |
| P2093 | author name string | Russell N. Pysklywec | |
| Marcia C. L. Quintas | |||
| P2860 | cites work | Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications | Q30040418 |
| Cretaceous vertical motion of australia and the australian- antarctic discordance | Q43526292 | ||
| Preliminary reference Earth model | Q55868389 | ||
| Tilting of continental interiors by the dynamical effects of subduction | Q56287617 | ||
| Some remarks on the development of sedimentary basins | Q56523482 | ||
| Effect of depth-dependent viscosity on the planform of mantle convection | Q57405645 | ||
| Intermittent layered convection in a model mantle with an endothermic phase change at 670 km | Q59051540 | ||
| Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle | Q59056430 | ||
| Complex morphology of subducted lithosphere in the mantle beneath the Tonga trench | Q59099364 | ||
| A reassessment of the heat transport by variable viscosity convection with plates and lids | Q59410160 | ||
| Locally layered convection inferred from dynamic models of the Earth's mantle | Q60075454 | ||
| Subducting slabs stagnant in the mantle transition zone | Q60568852 | ||
| Glacial geologic confirmation of an intraplate boundary, in the Paraná basin of Brazil | Q61662177 | ||
| Depressed continental hypsometry behind oceanic trenches: A clue to subduction controls on sea-level change | Q61662307 | ||
| Cenozoic subsidence and uplift of continents from time-varying dynamic topography | Q67211749 | ||
| Constraints on the vertical motion of eastern Australia during the Mesozoic | Q67659365 | ||
| Migration of glacial centers across Gondwana during Paleozoic Era | Q73804442 | ||
| Late Paleozoic to Triassic evolution of the Gondwana margin: Evidence from Chilean Frontal Cordilleran batholiths (28°S to 31°S) | Q73805501 | ||
| The Role of Subduction‐Induced Subsidence in the Evolution of the Karoo Basin | Q74092235 | ||
| Mantle convection with plates and mobile, faulted plate margins | Q81125369 | ||
| Rapid continental subsidence following the initiation and evolution of subduction | Q81144373 | ||
| Role of the lithosphere in mantle convection | Q97999096 | ||
| P433 | issue | B7 | |
| P921 | main subject | Paleozoic | Q75507 |
| P304 | page(s) | 16359-16370 | |
| P577 | publication date | 2000-07-10 | |
| P1433 | published in | Journal of Geophysical Research | Q2738009 |
| P1476 | title | A mantle flow mechanism for the late Paleozoic subsidence of the Paraná Basin | |
| P478 | volume | 105 |
| Q57977532 | Deep crustal structure of the Paraná Basin from receiver functions and Rayleigh-wave dispersion: Evidence for a fragmented cratonic root |
| Q60709976 | Multi-objective inversion of surface waves and receiver functions by competent genetic algorithm applied to the crustal structure of the Paraná Basin, SE Brazil |
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