Numerical modelling of crustal growth in intraoceanic volcanic arcs

By K. Nikolaeva, Taras V. Gerya, J. A. Connolly. 2008

161 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/691983f3f51aa614d72af1fd7679f475e7ea6d44

Citations in the corpus

• Three-dimensional thermomechanical modeling of oceanic spreading initiation and evolution (2013, unknown): “The total amount of melt, M, for every marker takes into account the amount of previously extracted melt and is calculated as (Nikolaeva et al., 2008) M ¼ M0 Rn Mext ð2Þ where Rn Mext is the total melt fraction extracted during the previous n extraction episodes.”
• Subduction styles in the Precambrian: Insight from numerical experiments (2009, unknown): “We also tested how the transition between the “modern subduction” regime and the “pre-subduction” regime is affected by a density contrast between the continental and the oceanic lithospheric mantle (Poudjom Djomani et al., 2001; Niu et al., 2003).”