Basin-scale structure, without the basin-scale survey.

Non-invasively image basin-wide earth structure to over 10,000 ft (3,200 m) depth, to assist in developing drill targets for producing energy resources in commercial quantities.

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Energy & Geothermal

Decades of geothermal experience behind the method.

Terēan®’s leadership has applied seismic imaging to geothermal exploration for decades — from SeisOpt® and ReMi® development at Optim to fieldwork with the Nevada Seismological Laboratory and Chevron’s exploration imaging.

Deep ReMi® characterizes shear-velocity sections down to geophysical basement using overlapping subsets of instruments, defining the lateral changes that reveal basin structure and geometry — the context you need before committing to a drill target.

10,000+ ft

Basin-wide structural imaging (3,200 m)

1 km

Deep ReMi® to geophysical basement

Passive

Ambient noise as the energy source

What you can see

ReMi® for energy & geothermal.

Basin structure & geometry

Define lateral velocity changes that reveal basin shape and depth to basement.

Fault imaging

Locate faults and structural controls relevant to fluid pathways.

Drill-target development

Use velocity structure to help prioritize where to drill.

Large arrays

Scale from 24 channels to 120+ channels and DAS fiber.

VsSurf ReMi 2dS® — Deep ReMi® 1,000+ ft — Deep ReMi® imaging of velocity structure beyond 1,000 ft.

…deep ReMi can characterize shear-velocity sections down to geophysical basement at 1 km depth, using overlapping subsets of instruments and defining lateral changes that allow derivation of basin structure and geometry.

Pancha, A., et al.Bulletin of the Seismological Society of America, 2017

Where to start