Year |
Citation |
Score |
2012 |
Spasojevic S, Gurnis M. Sea level and vertical motion of continents from dynamic earth models since the late cretaceous Aapg Bulletin. 96: 2037-2064. DOI: 10.1306/03261211121 |
0.648 |
|
2012 |
Gurnis M, Turner M, Zahirovic S, DiCaprio L, Spasojevic S, Müller RD, Boyden J, Seton M, Manea VC, Bower DJ. Plate tectonic reconstructions with continuously closing plates Computers and Geosciences. 38: 35-42. DOI: 10.1016/J.Cageo.2011.04.014 |
0.602 |
|
2010 |
Sutherland R, Spasojevic S, Gurnis M. Mantle upwelling after Gondwana subduction death explains anomalous topography and subsidence histories of eastern New Zealand and west Antarctica Geology. 38: 155-158. DOI: 10.1130/G30613.1 |
0.657 |
|
2010 |
Spasojevic S, Gurnis M, Sutherland R. Mantle upwellings above slab graveyards linked to the global geoid lows Nature Geoscience. 3: 435-438. DOI: 10.1038/Ngeo855 |
0.681 |
|
2010 |
Spasojevic S, Gurnis M, Sutherland R. Inferring mantle properties with an evolving dynamic model of the Antarctica-New Zealand region from the Late Cretaceous Journal of Geophysical Research: Solid Earth. 115. DOI: 10.1029/2009Jb006612 |
0.659 |
|
2009 |
Spasojevic S, Liu L, Gurnis M. Adjoint models of mantle convection with seismic, plate motion, and stratigraphic constraints: North America since the Late Cretaceous Geochemistry, Geophysics, Geosystems. 10. DOI: 10.1029/2008Gc002345 |
0.709 |
|
2008 |
Liu L, Spasojevic S, Gurnis M. Reconstructing Farallon plate subduction beneath North America back to the Late Cretaceous. Science (New York, N.Y.). 322: 934-8. PMID 18988850 DOI: 10.1126/Science.1162921 |
0.7 |
|
2008 |
Spasojević S, Liu L, Gurnis M, Müller RD. The case for dynamic subsidence of the U.S. east coast since the Eocene Geophysical Research Letters. 35. DOI: 10.1029/2008Gl033511 |
0.65 |
|
2008 |
Spasojević S, Clayton RW. Crustal structure and apparent tectonic underplating from receiver function analysis in South Island, New Zealand Journal of Geophysical Research. 113. DOI: 10.1029/2007Jb005166 |
0.55 |
|
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