Structural Geology of Parautochthonous and Allochthonous Terranes of the Penokean Orogeny in Upper Michigan

Structural Geology of Parautochthonous and Allochthonous Terranes of the Penokean Orogeny in Upper Michigan PDF Author: William J. Gregg
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 36

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Structural Geology of Parautochthonous and Allochthonous Terranes of the Penokean Orogeny in Upper Michigan

Structural Geology of Parautochthonous and Allochthonous Terranes of the Penokean Orogeny in Upper Michigan PDF Author: William J. Gregg
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 36

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Structural Geology of Parautochthonous and Allochthonous Terranes of the Penokean Orogeny in Upper Michigan

Structural Geology of Parautochthonous and Allochthonous Terranes of the Penokean Orogeny in Upper Michigan PDF Author: William J. Gregg
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 28

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Archean and Early Proterozoic Tectonic Framework of North-Central United States and Adjacent Canada

Archean and Early Proterozoic Tectonic Framework of North-Central United States and Adjacent Canada PDF Author: Paul Kibler Sims
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 20

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U.S. Geological Survey Bulletin

U.S. Geological Survey Bulletin PDF Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 372

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U.S. Geological Survey Bulletin

U.S. Geological Survey Bulletin PDF Author: Paul Kibler Sims
Publisher:
ISBN:
Category : Faults (Geology)
Languages : en
Pages : 268

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The Early Proterozoic Michigamme Formation of northern Michigan was deposited in the southeastern part of the Animikie basin. The formation conformably overlies the Goodrich Quartzite and comprises three widespread members a lower member of thin-bedded shale, siltstone, and sandstone; the Bijiki Iron-formation Member; and an upper member of tur- biditic graywacke, siltstone, and mudstone and a few local members. The Goodrich Quartzite is interpreted as having been deposited in a tidally influenced shallow marine environ- ment. The lower member of the Michigamme is interpreted as having been deposited in a tidally influenced environment, the iron-formation member as having been deposited below wave base in somewhat deeper water, and the upper member as having been deposited in still deeper water with turbidity currents being a major depositional mechanism. Several lines of evidence including paleocurrents, paleo- geographic setting, and neodymium isotopes suggest that the graywacke of the southern part of the outcrop area was derived from the south (Early Proterozoic Wisconsin magmatic terranes, Archean miniplates, and older Early Proterozoic sedimentary units formed on the continental margin), and that the graywacke in the northern area was derived from an Archean terrane to the north. The tectonic model that best fits the available data is a northward-migrating foreland basin.

Monthly Catalog of United States Government Publications

Monthly Catalog of United States Government Publications PDF Author:
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ISBN:
Category : Government publications
Languages : en
Pages :

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Monthly Catalogue, United States Public Documents

Monthly Catalogue, United States Public Documents PDF Author:
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 952

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Gneiss Domes in Orogeny

Gneiss Domes in Orogeny PDF Author: Donna Whitney
Publisher: Geological Society of America
ISBN: 0813723809
Category : Science
Languages : en
Pages : 404

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New Publications of the U.S. Geological Survey

New Publications of the U.S. Geological Survey PDF Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 370

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New Publications of the U.S. Geological Survey

New Publications of the U.S. Geological Survey PDF Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 64

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