A fi xed sublithospheric source for the late Neogene track of the Yellowstone hotspot : Implications of the Heise and Picabo volcanic fi elds

@inproceedings{Anders2014AFX,
  title={A fi xed sublithospheric source for the late Neogene track of the Yellowstone hotspot : Implications of the Heise and Picabo volcanic fi elds},
  author={M. D. Hans-Joachim Anders and David W. Rodgers and Sidney R. Hemming and Janet Saltzman and Victor J. DiVenere and Jonathan T Hagstrum and Glenn F. Embree and Robert C. Walter},
  year={2014}
}
The Heise and Picabo volcanic fields of eastern Idaho are part of the more extensive time-transgressive Yellowstone-Snake River Plain hotspot track. Calderas associated with these two silicic volcanic fields are buried under 1 to 3 km of younger basalt, so their locations and eruption record histories have been based on analysis of silicic units along the margins of the eastern Snake River Plain along with some limited geophysical data. A 1.5 km borehole penetrating through basalt into… CONTINUE READING
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