Reevaluation of the Piermont-Frontenac allochthon in the Upper Connecticut Valley: Restoration of a coherent Boundary Mountains-Bronson Hill stratigraphic sequence

Rankin, Douglas WTucker, R.D.Amelin, Yuri2015-12-080016-7606http://hdl.handle.net/1885/31943The regional extent and mode and time of emplacement of the Piermont-Frontenac alloch thon in the Boundary Mountains-Bronson Hill anticlinorium of the Upper Connecticut Valley, New Hampshire-Vermont, are controversial. Moench and coworkers beginning in thKeywords: Coherent boundaries; High resolution; New Hampshire; Silurian-Devonian; Stratigraphic sequences; Stratigraphic units; Synsedimentary; Thermal ionization mass spectrometry; Lead; Rivers; Silicate minerals; Stratigraphy; Landforms; allochthon; anticline; auReevaluation of the Piermont-Frontenac allochthon in the Upper Connecticut Valley: Restoration of a coherent Boundary Mountains-Bronson Hill stratigraphic sequence201210.1130/B30590.12016-02-24