Samovar: a thermomechanical code for modeling of geodynamic processes in the lithosphere – application to basin evolution

TY - CHAP

T1 - Samovar

T2 - a thermomechanical code for modeling of geodynamic processes in the lithosphere – application to basin evolution

AU - Elesin, Yuriy

AU - Gerya, Taras

AU - Artemieva, Irina

AU - Thybo, Hans

N1 - Reprinted from Arab J Geosci (2010) 3:477–497

PY - 2013

Y1 - 2013

N2 - We present a new 2D finite difference code, Samovar, for high-resolution numerical modeling of complex geodynamic processes. Examples are collision of lithospheric plates (including mountain building and subduction) and lithosphere extension (including formation of sedimentary basins, regions of extended crust, and rift zones). The code models deformation of the lithosphere with viscoelastoplastic rheology, including erosion/sedimentation processes and formation of shear zones in areas of high stresses. It also models steady-state and transient conductive and advective thermal processes including partial melting and magma transport in the lithosphere. The thermal and mechanical parts of the code are tested for a series of physical problems with analytical solutions. We apply the code to geodynamic modeling by examining mmierically the processes of lithosphere extension and basin formation. The results are directly apphcable to the Basin and Range province, western USA, and demonstrate the roles of crust-mantle coupling, preexisting weakness zones, and erosion rate on the evolutionary trends of extending continental regions. Modeling of basin evolution indicates a critical role of syn-rift sedimentation the depth of rift basins by preventing faulting in the subcrustal lithosphere.

AB - We present a new 2D finite difference code, Samovar, for high-resolution numerical modeling of complex geodynamic processes. Examples are collision of lithospheric plates (including mountain building and subduction) and lithosphere extension (including formation of sedimentary basins, regions of extended crust, and rift zones). The code models deformation of the lithosphere with viscoelastoplastic rheology, including erosion/sedimentation processes and formation of shear zones in areas of high stresses. It also models steady-state and transient conductive and advective thermal processes including partial melting and magma transport in the lithosphere. The thermal and mechanical parts of the code are tested for a series of physical problems with analytical solutions. We apply the code to geodynamic modeling by examining mmierically the processes of lithosphere extension and basin formation. The results are directly apphcable to the Basin and Range province, western USA, and demonstrate the roles of crust-mantle coupling, preexisting weakness zones, and erosion rate on the evolutionary trends of extending continental regions. Modeling of basin evolution indicates a critical role of syn-rift sedimentation the depth of rift basins by preventing faulting in the subcrustal lithosphere.

U2 - 10.1007/978-3-642-30609-9_22

DO - 10.1007/978-3-642-30609-9_22

M3 - Book chapter

SN - 978-3-642-29278-1

T3 - Frontiers in Earth Sciences

SP - 441

EP - 461

BT - Lithosphere dynamics and sedimentary basins

A2 - Hosani, K.A.

A2 - Roure, F.

A2 - Ellison, R.

A2 - Lokier, S.

PB - Springer Publishing Company

ER -