Show simple item record

dc.contributor.advisorMahoney, J. Brian
dc.contributor.advisorPignotta, Geoffrey S.
dc.contributor.advisorIhinger, Phillip D.
dc.contributor.authorKing, Nicholas E.
dc.contributor.authorBalgord, Elizabeth A.
dc.contributor.authorKadulski, Brennan M.
dc.contributor.authorMeyers, Jessica L.
dc.contributor.authorPotter, Julia J.
dc.descriptionColor poster with text, charts, and maps.en
dc.description.abstractSouthwest Montana experienced large-scale magmatism and regional contraction during the Late Cretaceous. Understanding the genetic linkages between these geologic processes is important for understanding the causes of mountain-building in the Cordillera. Our analysis of the field relationships between the Boulder magmatic system and the folded Paleozoic rocks constrain the sequence of events that shaped the tectonomagmatic evolution of the Helena salient.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programsen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectBoulder Batholith (Mont.)en
dc.titleGeologic Analysis of the Northern Margin of the Boulder Batholith II : Geologic Map of the Esmerelda Hills Quadrangleen

Files in this item


This item appears in the following Collection(s)

  • Student Research Day
    Posters of collaborative student/faculty research presented at Student Research Day

Show simple item record