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Home > Society and Social Sciences > Politics and government > The Gogebic Iron Range: A Sample of the Northern Margin of the Penokean Fold and Thrust Belt: Usgs Professional Paper 1730(English)
The Gogebic Iron Range: A Sample of the Northern Margin of the Penokean Fold and Thrust Belt: Usgs Professional Paper 1730(English)

The Gogebic Iron Range: A Sample of the Northern Margin of the Penokean Fold and Thrust Belt: Usgs Professional Paper 1730(English)

          
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About the Book

The Gogebic iron range is an elongate belt of Paleoproterozoic strata extending from the west shore of Lake Gogebic in the upper peninsula of Michigan for about 125 km westward into northern Wisconsin. It is one of six major informally named iron ranges in the Lake Superior region and produced about 325 million tons of direct-shipping ore between 1887 and 1967. A significant resource of concentrating-grade ore remains in the western and eastern parts of the range. The iron range forms a broad, gently southward-opening arc where the central part of the range exposes rocks that were deposited somewhat north of the eastern and western parts. A fundamental boundary marking both the tectonic setting of deposition and the later deformation within the Penokean orogen lies fortuitously in an east-west direction along the range so that the central part of the range preserves sediments deposited north of that boundary, whereas the eastern and western parts of the range were deposited south of the boundary. Thus, the central part of the range provides a record of sedimentation and very mild deformation in a part of the Penokean orogen farthest from the interior of the orogen to the south. The eastern and western parts of the range, in contrast, exhibit a depositional and deformational style typical of parts closer to the interior of the orogen. A second fortuitous feature of the iron range is that the entire area was tilted from 40 to 90 northward by Mesoproterozoic deformation so that the map view offers an oblique cross section of the Paleoproterozoic sedimentary sequence and structures. Together, these features make the Gogebic iron range a unique area in which to observe (1) the lateral transition from deposition on a stable platform to deposition in a tectonically and volcanically active region, and (2) the transition from essentially undeformed Paleoproterozoic strata to their folded and faulted equivalents.


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Product Details
  • ISBN-13: 9781287031192
  • Publisher: Bibliogov
  • Publisher Imprint: Bibliogov
  • Height: 246 mm
  • No of Pages: 58
  • Series Title: English
  • Sub Title: A Sample of the Northern Margin of the Penokean Fold and Thrust Belt: Usgs Professional Paper 1730
  • Width: 189 mm
  • ISBN-10: 1287031196
  • Publisher Date: 01 Apr 2013
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Spine Width: 3 mm
  • Weight: 122 gr


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