Romberger's (1992) paper suggests that deposition of 500 tonnes of gol
d in six unusually rich Nevada deposits was due to normal ore-bearing
solutions flowing at a more rapid rate and for a longer period of time
than usual through well-developed channels perpetuated by continual b
recciation. It is now understood that plate tectonics requires that 15
million years ago the Yellowstone mantle plume should have formed and
begun to migrate eastward relative to the North American plate at a r
ate of approximately 35 km per million years. This paper proposes that
the passage of the plume past the deposits coincided with the time of
ore deposition, indicating that the plume was a factor in forming the
ore bodies. It mentions some other reasons why plumes should be taken
into account in economic geology