The present disclosure relates to a method for identifying the distance of
sediment source in a fault basin based on
well logging data, which analyzes the paleocurrent by using the imaging
logging data, determines the direction of the paleocurrent, and then scales the imaging
logging, conventional
logging and nuclear magnetic logging by using the core, determines the conventional logging
response characteristics, nuclear magnetic T2 distribution spectrum characteristics of the far source, medium source and near source, establishes the source distance identification chart, realizes the longitudinal continuous, efficient, accurate and low-cost
sediment source distance discrimination, and provides an important basis for the analysis of the
sediment basin; the present disclosure analyzes the distance of the sediment source based on the
well logging data, fully excavates the geological information of the existing
well logging data, reduces the cost to the minimum, and solves the problems of the discontinuity of the source distance determined by using the core data, and the low accuracy of the source analysis result when the core data is insufficient.