StructureTHERE IS A SLIGHT REGIONAL DIP, 16 FT/MI (3.03 M/KM), TO THE NORTH NORTHEAST AND THE AXIS OF THE DAKOTA (WILLISTON) BASIN. SUPERIMPOSED UPON THIS REGIONAL STRUCTURE ARE SMALL SECONDARY FAULTS AND FOLDS WITH AMPLITUDES AND DISPLACEMENTS OF LESS THAN 20 FT (6.10 M).
Economic & production
Development statusProducer
Identification
Deposit ID60001234
MRDS IDSD01097
RegionNA
Data scoreD
Coordinates45.84636, -102.37554
References
STEVENSON, ROBERT E., 1954, HAYNES QUAD, SOUTH DAKOTA GEOLOGICAL SURVEY