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Found 10 records similar to Noranda seismic; Line rbg00001; 2D seismic reflection
The GSC obtained access to industry-owned seismic reflection data along two profiles crossing volcanic rocks of the Noranda mining camp. The integration of seismic data and 3-D geological provides new constraints on the deep geological framework.
The GSC obtained access to industry-owned seismic reflection data along two profiles crossing volcanic rocks of the Noranda mining camp. The integration of seismic data and 3-D geological provides new constraints on the deep geological framework.
In 1998 Noranda Mining and Exploration collected a 2D side-swipe survey in the vicinity of the Heath Steele mining camp in New Brunswick. The objective of the experiment was to examine the possibility of using 2D seismic techniques to image reflected/scattered energy from vertically dipping stratigraphy.
In 1997, Noranda acquired a 7.8 km seismic line in the vicinity of the Sturgeon Lake mining camp in Norwestern Ontario. Data processing was performed at the GSC and the dynamite data displayed high signal levels with strong reflectivity observed at depth.
Exploration for new base metal deposits in the Brunswick camp required focused investigation of geological structures at depth. For this reason, seismic reflection data in the Brunswick No. 6 area were acquired along three 2D profiles in 1999, with a total length of about 30 km and followed by an about 38-km2 3D data set over the area.
Exploration for new base metal deposits in the Brunswick camp required focused investigation of geological structures at depth. For this reason, seismic reflection data in the Brunswick No. 6 area were acquired along three 2D profiles in 1999, with a total length of about 30 km and followed by an about 38-km2 3D data set over the area.
Exploration for new base metal deposits in the Brunswick camp required focused investigation of geological structures at depth. For this reason, seismic reflection data in the Brunswick No. 6 area were acquired along three 2D profiles in 1999, with a total length of about 30 km and followed by an about 38-km2 3D data set over the area.
Three high-resolution vibroseis reflection profiles were acquired across the Paleoproterozoic Huronian Supergroup (2.5-2.2 Ga) of the Canadian Shield, in the vicinity of the Temagami Lake magnetic anomaly. Quality seismic images reveal a 20-km-wide early Proterozoic rift basin beneath a thick cover of metasidiments.
Three high-resolution vibroseis reflection profiles were acquired across the Paleoproterozoic Huronian Supergroup (2.5-2.2 Ga) of the Canadian Shield, in the vicinity of the Temagami Lake magnetic anomaly. Quality seismic images reveal a 20-km-wide early Proterozoic rift basin beneath a thick cover of metasidiments.
Three high-resolution vibroseis reflection profiles were acquired across the Paleoproterozoic Huronian Supergroup (2.5-2.2 Ga) of the Canadian Shield, in the vicinity of the Temagami Lake magnetic anomaly. Quality seismic images reveal a 20-km-wide early Proterozoic rift basin beneath a thick cover of metasidiments.