Modeling mobile shales under contraction: Critical analyses of new analog simulations of shale tectonics and comparison with salt-bearing systems

Author:

Dooley Tim P.1ORCID,Soto Juan I.2ORCID,Reber Jacqueline E.3ORCID,Hudec Michael R.4ORCID,Peel Frank J.4ORCID,Apps Gillian M.4ORCID

Affiliation:

1. The University of Texas at Austin, Bureau of Economic Geology, Jackson School of Geoscience, Austin, Texas, USA. (corresponding author)

2. The University of Texas at Austin, Bureau of Economic Geology, Jackson School of Geoscience, Austin, Texas, USA and Granada University, Departamento de Geodinámica, Granada, Spain. ,

3. Iowa State University, Department of Earth, Atmosphere, and Climate, Ames, Iowa, USA.

4. The University of Texas at Austin, Bureau of Economic Geology, Jackson School of Geoscience, Austin, Texas, USA.

Abstract

Weak substrates, such as salt and mobile shales, exert a strong control on deformation styles in all structural settings, especially those undergoing contraction. Despite both materials being very weak, they are mechanically very different. Salt is weak and will flow in a ductile fashion under most geologic conditions, whereas shales only become mobile after reaching a critical state. Many sandbox-style physical or analog modeling studies have typically used a salt analog, viscous silicone polymer, as a proxy for mobile shales. However, to more accurately model mobile shale behavior, the model material needs to exhibit yield strength. One such material is Carbopol, which is made up of microgel grains that are elasto-plastic, separated by a viscous interstitial fluid. The abundance of the grains depends on the concentration of the mixture. Our results show that Carbopol does behave much differently than the traditional salt analog during contraction. Polydimethylsiloxanes typically undergoes bulk deformation and inflation under contraction, whereas Carbopol forms discrete, intense shear zones and contains zones of little to no strain where its yield strength has not been exceeded. Below the shale analog, brittle layers typically form imbricate thrust stacks, jacking up the overburden, with shear zones propagating out from thrust tips along and through the shale proxy. Strain analyses reveal complex switching of activity within the Carbopol and overlying sediments. Models reveal that even a very thin layer of Carbopol can act as a highly efficient detachment, and form more geologically realistic shortening structures, especially where these detachments are vertically stacked and horizontally offset. We believe that Carbopol is a powerful mobile-shale analog and opens new modeling directions because, as far as we are aware, this material has never been incorporated into a traditional sandbox model. Future work will seek to incorporate this material into more complex and 3D sandbox-style models.

Funder

Applied Geodynamics Laboratory Industrial Associates program

Bureau of Economic Geology, University of Texas at Austin

Jackson School of Geosciences, The University of Texas at Austin

Publisher

Society of Exploration Geophysicists

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