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Finite Strain in the Precambrian Kona Formation, Marquette County, Michigan

Author: David B. Westjohn
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 168

Book Description

Finite Strain in the Precambrian Kona Formation, Marquette County, Michigan

Author: David B. Westjohn
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 168

Book Description

A Strain Study in the Kona Formation, Marquette County, Michigan

Author: Rudolf Meyer
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 156

Book Description

Regional Finite Strain Patterns in Proterozoic Slates and Quartzites

Author: David B. Westjohn
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 416

Book Description

U.S. Geological Survey Bulletin

Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 372

Book Description

U.S. Geological Survey Bulletin

Author: Paul Kibler Sims
Publisher:
ISBN:
Category : Faults (Geology)
Languages : en
Pages : 268

Book Description
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.