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lines changed Original file line number Diff line number Diff line change @@ -22,7 +22,7 @@ where $\epsilon$ controls the viscosity contrast. It is easy to verify that
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the flow is incompressible as the velocity field satisfies
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$\nabla\cdot \mathbf u = 0$. The right hand side term of the Stokes equation
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is obtained by inserting the expressions for velocity, pressure and viscosity
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- in the momentum conservation equation, see {cite: t }` thieulot:2019 ` for details. The
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+ in the momentum conservation equation, see {cite: t }` fieldstone ` for details. The
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velocity, pressure and right hand side magnitude are shown in {numref}` fig:benchmark-grooves-3x3 `
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for $L=3$ and $\epsilon=0.1$.
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Original file line number Diff line number Diff line change @@ -11855,11 +11855,11 @@ @article{garzanti:etal:2018
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doi = { 10.1016/j.earscirev.2017.11.012} ,
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}
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- @Misc { thieulot:2019 ,
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- author = { C. Thieulot} ,
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- title = { The Finite Element Method in Geodynamics } ,
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- url = { https://github.com/cedrict/fieldstone/blob/master/manual.pdf } ,
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- year = { 2019 }
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+ @misc { fieldstone ,
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+ author = " Cedric Thieulot" ,
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+ title = " {Fieldstone: a computational geodynamics (self-)teaching tool} " ,
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+ year = " 2023 " ,
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+ url = { https://cedrict.github.io/ }
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}
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@incollection {john:knobloch:2006 ,
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