How can we get information about the stress field near the surface? Some kilometers down? Even deeper down?

What will be an ideal response?


Answer: Near the surface: Overcoring measurements, but also the orientation of recent fractures or fault scarps from earthquakes, fold axes and fissures associated with volcanism can indicate the orientation of the least horizontal principal stress. Some kilometers down (in wells): Borehole breakouts estimated from dipmeter or well imaging tools, hydraulic fracturing, overcoring (less common and more difficult). Deeper down focal mechanisms give stress information.

Environmental & Atmospheric Sciences

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Environmental & Atmospheric Sciences