شذوذ تِماگامي المغناطيسي

Landsat image showing the anomaly, cross is at the centre of it. Shows the terrain only, not the magnetic deviations of the area.

شذوذ تـِماگامي المغناطيسي Temagami Magnetic Anomaly، ويُدعى أيضاً شذوذ تماجامي أو شذوذ واناپيتـِيْ Wanapitei Anomaly، هو شذوذ مغناطيسي ينتُج عن بنية جيولوجية كبيرة مدفونة في الدرع الكندي بالقرب من Temagami, Ontario, Canada. It stretches from Lake Wanapitei in the west to Bear Island in Lake Temagami.

The Aboriginal community of Teme-Augama Anishnabai lies partly within the Temagami Magnetic Anomaly, including the Temagami First Nation on Bear Island. Located nearby are a number of other geological structures, including the Sudbury Basin, the Lake Wanapitei impact crater, and the Temagami Greenstone Belt.

. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

الاكتشاف والبنية

The Anomaly on a map, the larger pink spot near the center of the image.

The Temagami Magnetic Anomaly is egg-shaped, 58 km (36 mi) long and 19 km (12 mi) wide. The central section has the greatest amplitude and an east–west strike.

The western portion appears smoother in character while the eastern section is long and narrow. With an areal extent of 50 x 15 km, it reaches a magnitude of approximately 10,000 nanoteslas, making it one of the largest positive anomalies in North America.^[1] The eastern section coincides with a small positive gravity anomaly, indicating the presence of dense rocks at depth.^[2] The anomaly was discovered by a magnetic survey and a gravity survey.

انظر أيضاً

المراجع

^ Pilkington, Mark (1997). 3-D Magnetic Imaging using Conjugate Gradients: Temagami anomaly Geophysics, Vol. 62, No. 4 (July–August 1997).
^ Kawohl, Alexander et al. (2017).What's inside the Temagami geophysical anomaly, Sudbury District, Ontario? SGA Québec 2017 extended abstract, Vol. 4, 1543-1546.

47°00′N 80°12′W / 47.0°N 80.2°W / 47.0; -80.2 (Temagami magnetic anomaly)

[1] Pilkington, Mark (1997). 3-D Magnetic Imaging using Conjugate Gradients: Temagami anomaly Geophysics, Vol. 62, No. 4 (July–August 1997).

[2] Kawohl, Alexander et al. (2017).What's inside the Temagami geophysical anomaly, Sudbury District, Ontario? SGA Québec 2017 extended abstract, Vol. 4, 1543-1546.

[1]

[2]