The geometry and stresses of a fault zone often determine where fractures start, how they grow, and where they stop. In a new study¹, we used deep-learning polarity picks and SKHASH to build a dense catalog of over 16,000 well-constrained
The geometry and stresses of a fault zone often determine where fractures start, how they grow, and where they stop. In a new study¹, we used deep-learning polarity picks and SKHASH to build a dense catalog of over 16,000 well-constrained