Articles | Volume 11, issue 1
Geosci. Model Dev., 11, 43–60, 2018
https://doi.org/10.5194/gmd-11-43-2018
Geosci. Model Dev., 11, 43–60, 2018
https://doi.org/10.5194/gmd-11-43-2018

Model description paper 05 Jan 2018

Model description paper | 05 Jan 2018

SILLi 1.0: a 1-D numerical tool quantifying the thermal effects of sill intrusions

Karthik Iyer et al.

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Cited articles

Aarnes, I., Svensen, H., Connolly, J. A. D., and Podladchikov, Y. Y.: How contact metamorphism can trigger global climate changes: Modeling gas generation around igneous sills in sedimentary basins, Geochim. Cosmochim. Ac., 74, 7179–7195, 2010. 
Aarnes, I., Fristad, K., Planke, S., and Svensen, H.: The impact of host-rock composition on devolatilization of sedimentary rocks during contact metamorphism around mafic sheet intrusions, Geochem. Geophy. Geosy., 12, Q10019, https://doi.org/10.1029/2011GC003636, 2011a. 
Aarnes, I., Svensen, H., Polteau, S., and Planke, S.: Contact metamorphic devolatilization of shales in the Karoo Basin, South Africa, and the effects of multiple sill intrusions, Chem. Geol., 281, 181–194, 2011b. 
Aarnes, I., Planke, S., Trulsvik, M., and Svensen, H.: Contact metamorphism and thermogenic gas generation in the Vøring and Møre basins, offshore Norway, during the Paleocene–Eocene thermal maximum, J. Geol. Soc., 172, 588–598, https://doi.org/10.1144/jgs2014-098, 2015. 
Archer, S. G., Bergman, S. C., Iliffe, J., Murphy, C. M., and Thornton, M.: Palaeogene igneous rocks reveal new insights into the geodynamic evolution and petroleum potential of the Rockall Trough, NE Atlantic Margin, Basin Res., 17, 171–201, 2005. 
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Igneous intrusions in sedimentary basins have a profound effect on the thermal structure of the hosting sedimentary rocks. In this paper, we present a user-friendly 1-D FEM-based tool, SILLi, that calculates the thermal effects of sill intrusions on the enclosing sedimentary stratigraphy. The motivation is to make a standardized numerical toolkit openly available that can be widely used by scientists with different backgrounds to test the effects of magmatic bodies in a wide variety of settings.