|Title||Interpretations of gravimetric and magnetic anomalies on traverses in the Canadian Shield in northern Ontario|
|Author||Garland, G D|
|Source||Publications of the Dominion Observatory vol. 16, no. 1, 1950, 55 pages (1 sheet), https://doi.org/10.4095/8672|
|Publisher||Canada Department of Mines and Technical Surveys (Ottawa, Canada)|
|Maps||Publication contains 1 map|
|Map Info.||geophysical, gravity anomalies, 1:1,900,800|
|Media||paper; on-line; digital|
|NTS||31 /NW; 31 /SE; 31 /SW; 32D; 41 /NE; 41 /SE; 42 /NE; 42 /SE; 43 /NE; 43 /SE|
|Subjects||geophysics; regional geology; structural geology; basalts; conglomerates; gneisses; granites; granitic rocks; gravity interpretations; greywackes; magnetic interpretations; quartzites; magnetic surveys,
ground; gravity surveys, ground; Canadian Shield; Grenville Province; Kapuskasing-fraserdale High; Keewatin Volcanics; Matachewan-guerin Low; Mattawa Low; New Liskeard-cochrane Traverse; Port Arthur Low; Port Arthur-man Boundary Trav; Sudbury High;
Timiskaming Sediments; Ville Marie Traverse; Precambrian|
|Illustrations||schematic diagrams; geophysical profiles; geoscientific sketch maps; tables; cross-sections|
Natural Resources Canada Library - Ottawa (Earth Sciences)
|Released||1950 01 01; 2018 10 09|
|Abstract||The Bouguer anomalies obtained on gravity traverses over the Canadian Shield in northern Ontario are separated into local and regional effects. The latter are evidently too extensive to be directly
attributed to surface formations, and apparently result from conditions deep within the crust. Two characteristic strike directions are exhibited by these regional trends, east-west and northeast-southwest, allowing them to be separated into two age
groups. The first (cast-west striking) group of structures apparently dates from early Precambrian times, as it closely parallels folding and thrust faulting in the Timiskaming sediments, while the second (northeast-southwest striking) group is
believed to result from tectonic activity of Huronian age.|
Interpretation of these anomalies has been based on the assumption of a layered crust, consisting of an upper, or granitic layer, underlain by a basaltic layer. It is shown that the
majority of the regional anomalies cannot be explained by structures at a depth as great as the base of the basaltic layer (36 kilometers), but could be caused by irregularities in the thickness of the granitic layer. For example, a marked gravity
low, indicating a thickened granitic layer, trends east-west just south of the Kirkland Lake thrust zone. It would appear that this represents the remnant of the root of an early Precambrian mountain range, as the surface rocks along the low are
dominantly granite, while Precambrian sediments and. volcanics are preserved north and south of the low. A second root structure is suggested along the northwest limit of the Grenville province, where a line of thrust mountains is believed to have
formed during Huronian time.
In contrast to these areas of low gravity, regions of relatively high anomaly are found to be largely covered by Precambrian sediments. The implication is that these regions were low basins in Precambrian times, so
that the surface rocks were preserved from the great erosion which bared such large masses of granite elsewhere.
The conclusion is, therefore, that irregularities in the granitic layer exist as a result of Precambrian mountain-building processes,
and that these irregularities produce the broad, regional gravity anomalies. A departure from isostatic equilibrium is thus indicated, since the root structures have long outlived the topographic features they once supported.
The more local
gravity anomalies of the Shield are found to have a direct correlation with the known surface geology. That is, small, well defined highs are observed over belts of relatively dense Keewatin lavas, with the geological contacts quite accurately
demarcated by the inflection points of the gravity profiles. By comparison of the observed curves with those calculated for type bodies, an estimate may be made of the depth to the base of the Keewatin rocks. Such estimates are of interest because of
the ore deposits found within the lavas. For some of the broader lava belts, depths up to ten thousand feet are indicated.