Since Vening‐Meinesz's realization that the East African Rift represented an extensional, not
compressional, feature and since the widespread acceptance of plate tectonics two decades …

A database consisting of 25 data-sets has been compiled that includes published chemical
analyses of most known eastern North American occurrences of late Neoproterozoic …

Mafic dikes of late Proterozoic age which cut Grenvillian crust in the northeastern
Adirondack Mountains are mostly mildly alkaline basalts except for a few tholeiitic examples …

The Pinney Hollow Formation of central Vermont is part of a rift-clastic to drift-stage
sequence of cover rocks deposited on the Laurentian margin during the development of the …

Geologic evidence of the Neoproterozoic rifting of Laurentia during breakup of Rodinia is
recorded in basement massifs of the cratonic margin by dike swarms, volcanic and plutonic …

The Caldwell Group belongs to the Internal Nappe Domain of the Humber Zone and
consists of basaltic lavas, quartzo-feldspathic sandstones, and mudslates. The lavas are …

Mafic rocks containing sodic-calcic amphibole in the Green Mountain slice (GMS) and
Rowe/Prospect Rock slice (R/PRS), Vermont Appalachians were originally subalkaline …

Metamorphosed mafic rocks from west-central Vermont crop out in tectonic slices of the
Stowe Formation within the Rowe–Hawley Belt of New England. The rocks include …

ABSTRACT The Vermont Appalachians expose metamorphosed magmatic rocks ranging in
age from Late Proterozoic to Cretaceous. Geochemistry, in concert with stratigraphic …

Greenstone bodies from the western Vermont Appalachians and dikes intruding the
Adirondack massif comprise metavolcanic rocks that originated as basalt formed during …