| CPC E21B 43/17 (2013.01) [E21B 2200/20 (2020.05)] | 24 Claims |

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1. A system comprising:
(a) an injector well extending from a surface to a subterranean geologic formation and configured to be perforated;
(b) a pump configured to produce a thermal lattice in the subterranean geologic formation by:
(i) pumping a first volume of one or more fluids capable of tensile fracturing the subterranean geologic formation, generating a downhole pressure that produces a stress on the subterranean geologic formation exceeding a minimum horizontal stress of the subterranean geologic formation, from the injector well to a producer well, the producer well extending from the surface to the subterranean geologic formation;
(ii) pumping the one or more fluids in a pulsing mode to cause fatigue to any existing natural fractures intersecting fractures caused by the tensile fracturing, or to natural non-fractured rock, the pulsing mode having a pulse amplitude below the minimum horizontal stress of the subterranean geologic formation with frequency determined by rock fabric of the subterranean geologic formation and bottom hole static temperature;
(iii) pumping a second volume of the one or more fluids during an injection period as a hydro-shearing stage, the second volume based on an estimated total porosity of natural fractures encountered in the subterranean geologic formation estimated from a borehole logging tool or from geologic settings of the subterranean geologic formation; and
(c) a measurement sub-system configured to measure enhanced connectivity or permeability or both of the subterranean geologic formation after creation of the thermal lattice.
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