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Crooked-line 2D seismic reflection imaging in crystalline terrains: Part 2, migration
(2003-01)
Seismic reflection surveys are frequently conducted over very complicated geological structure, but surveying often must be confined to existing crooked roads or tracks. Typically, data from such 2D crooked-line surveys ...
Field Trip A1: Contamination in the South Mountain Batholith and Port Mouton Pluton, southern Nova Scotia
(Atlantic Geoscience Society, 2003)
Crooked-line 2D seismic reflection imaging in crystalline terrains: Part 1, data processing
(2003-01)
For cost and access reasons, most of the seismic reflection data collected in crystalline terrains have been acquired by 2D crooked-line profiling. When the survey geometry is significantly irregular and the geologic ...
Evolution of orogenic wedges and continental plateaux: insights from crustal thermal-mechanical models overlying subducting mantle lithosphere
(2003-04)
The links between an early phase of orogenesis, when orogens are commonly wedge shaped, and a later phase, with a plateau geometry, are investigated using coupled thermal-mechanical models with uniform velocity subduction ...
Tidal sedimentation in the Cornwallis River - Avon River Estuaries, Bay of Fundy, Nova Scotia: sedimentology, morphology, and natural history
(Atlantic Geoscience Society, 2003)
Exploded xenoliths, layered granodiorites, and chaotic Schlieren associated with the eastern contact of the South Mountain Batholith
(Atlantic Geoscience Society, 2003)
Hidden Cretaceous basins in Nova Scotia
(Atlantic Geoscience Society, 2003)
Quaternary and late Pliocene seismic stratigraphy of the central Scotian Slope
(2003-04-15)
High resolution single channel seismic reflection profiles collected by the Geological Survey of Canada Atlantic (GSCA) have been used to define the Quaternary and Late Pliocene seismic stratigraphy of the central Scotian ...
llmenite-Pyrophanite and Niobian RuHle in tbe South Mountafn Batholith, Nova Scotia
(2003-04-15)
Ilmenite and rutile are ubiquitous, but modally scarce (<0.5%), minerals in gr~nitoid rocks of the differentiated peraluminous South Mountain Batholith (SMB). Ilmenite occurs as blocky 0.05-0.90 mm grains in biotite, and ...