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Geological Survey Professional Paper Volume 310; No. 1035, Pts. 1-3

Geological Survey Professional Paper Volume 310; No. 1035, Pts. 1-3


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1987* Excerpt: ... by gneissic granite. In general the anomalies are small and discontinuoubut do exhibit definite trends. Anomaly I), in the northwestern part of T. 41 N.. R. 30 W., is close to and roughly parallel to the southern border of the Felch trough. It appears to lie within the granite, although it is partly obscured by the strong d anomaly to the north. Anomalies D2 and D3, in sec. 1, T. 41 N., R. 30 W., and secs. 5 and 6, T. 41 N., R. 29 W., are well within the gneissic granite and, like D1? evidently are caused by magnetic zones in the granite complex. Anomaly D4 follows the southern contact of the narrow tongue of Animikie rocks that lie within the gneissic granite in the northern part of T. 41 N., R. 30 W. Its crest in the SW1/ sec. 10 lies between low outcrops of granite which are several hundred feet apart. A small patch of slightly magnetic granite pegmatite was found in one of these outcrops. About a half mile to the east, in the SE14 sec. 10, the crest is on the north slope of a prominent ridge of Sturgeon quartzite, although not directly over actual exposures of the rock. Some of this quartzite contains magnetite crystals, and hand specimens tested with the ground magnetometer are slightly magnetic. D4 is likely made up of more than one separate anomaly, as it seems due partly to magnetic material in the sediments and partly to magnetic zones in the granite. Anomaly D5, although small, appears to be continuous from sec. 12, T. 41 N., R. 30 W., for a distance of about 5 miles to sec. 11, T. 41 N., R. 29 W. It crosses the Toby Lake fault with no noticeable offset, which suggests it may be caused by a magnetic dike that was intruded after the major movement of the fault. The D6 group of small anomalies is scattered through the gneissic granite along a 7-m...


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Product Details
  • ISBN-13: 9781235900129
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 116
  • Spine Width: 6 mm
  • Width: 189 mm
  • ISBN-10: 1235900126
  • Publisher Date: 01 May 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 222 gr


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Geological Survey Professional Paper Volume 310; No. 1035, Pts. 1-3
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