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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Atlantic Ocean
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North Atlantic
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Gulf of Maine (3)
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Canada
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Primary terms
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Atlantic Ocean
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carbon
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Geochronology, geochemistry, and tectonic setting of Ordovician metavolcanic rocks in the Liberty–Orrington belt, Maine: implications for the evolution of peri-Gondwanan arcs in the northern Appalachians
Evaluation of a combined HRXCT/EBSD method for detecting epitaxial nucleation of garnet porphyroblasts
Statistical variability of the geochemistry and mineralogy of soils in the Maritime Provinces of Canada and part of the Northeast United States
COMPOSITIONAL AND STRUCTURAL VARIATIONS IN COLUMBITE-GROUP MINERALS FROM GRANITIC PEGMATITES OF THE BRUNSWICK AND OXFORD FIELDS, MAINE: DIFFERENTIAL TRENDS IN F-POOR AND F-RICH ENVIRONMENTS
The Dog Bay – Liberty Line and its significance for Silurian tectonics of the northern Appalachian orogen 1 This article is one of a series of papers published in this CJES Special Issue: In honour of Ward Neale on the theme of Appalachian and Grenvillian geology. 2 Geological Survey of Canada Contribution 20100257.
Assessing the role of orogen-parallel faulting in post-orogenic exhumation: low-temperature thermochronology across the Norumbega Fault System, Maine
A 1500 yr record of North Atlantic storm activity based on optically dated relict beach scarps
High-Resolution Subsurface (GPR) Imaging and Sedimentology of Coastal Ponds, Maine, U.S.A.: Implications for Holocene Back-Barrier Evolution
Late Cretaceous reactivation of the Norumbega fault zone, Maine: Evidence from apatite fission-track ages
Net ebb sediment transport in a rock-bound, mesotidal estuary during spring-freshet conditions: Kennebec River estuary, Maine
Sm-Nd isotope systematics and the derivation of granitic pegmatites in southwestern Maine
Nb-Ta-Ti oxides in granitic pegmatites from the Topsham pegmatite district, southern Maine
Stratigraphic evolution of the inner continental shelf in response to late Quaternary relative sea-level change, northwestern Gulf of Maine
Late Quaternary relative sea-level change in the western Gulf of Maine: Evidence for a migrating glacial forebulge
Contrasting thermal histories across the Flying Point fault, southwestern Maine: Evidence for Mesozoic displacement
Changing models of deglaciation in northern New England and adjacent Canada
Prior to about 1963 it was generally accepted that northern New England and adjacent Canada were progressively deglaciated from southeast to northwest during Late Pleistocene time. R. Chalmers and E. Antevs thought differently, but their views were not seriously considered, although their models were basically correct as we understand the deglaciation pattern today. Since about 1963 abundant evidence has accumulated that demonstrates that the Laurentide Ice Sheet was partitioned by a marine calving embayment that advanced up the St. Lawrence Lowland to the Ottawa area at least by 12,800 years B.P. This event left ice sheet remnants over much of Maine, southeastern Quebec, and probably in New Brunswick and western New England as well. Continuing research is needed to delineate the details of the final deglaciation in southeastern Quebec and Maine. Data presently available suggests that the Longfellow, White, and Boundary Mountains emerged as nunataks as early as 15,000 years ago, separating the ice sheet to the north and south. The Frontier Moraine, located on the divide between Quebec and Maine, formed at that time. Subsequently, other moraines formed as the margin of the ice sheet receded northwestward into the St. Lawrence Lowland of Quebec.