Elastic stress transmission and transformation (ESTT) by confined liquid: A new mechanics for fracture in elastic lithosphere of the earth
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Proposing a new fracture-forming mechanism that involves a confined liquid

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A confined liquid has the potential to produce tensile effective tangential stress.

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Dike propagates along the axes of cylindrical zones in non-tectonic regions.

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The minimum depth for liquid-driven fracture induced by a spherical liquid is 2–6 km.

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