Geochemistry and Petrology of the Nipissing Diabase in Ontario PDF Download
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Author: John Allison Colwell
Publisher:
ISBN:
Category : Geochemistry
Languages : en
Pages : 242
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Book Description
Author: John Allison Colwell
Publisher:
ISBN:
Category : Geochemistry
Languages : en
Pages : 242
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Book Description
Author: Peter Charles Lightfoot
Publisher: Ontario Ministry of Northern Development and Mines
ISBN: 9780777848043
Category : Science
Languages : en
Pages : 92
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Book Description
Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1178
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Book Description
Author:
Publisher: Natural Resources Canada
ISBN:
Category :
Languages : en
Pages : 59
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Book Description
Author: Ontario. Ministry of Natural Resources
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 316
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Book Description
Author: Canadian Institute of Mining, Metallurgy and Petroleum
Publisher:
ISBN:
Category : Platinum group
Languages : en
Pages : 872
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Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 372
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Book Description
Author: Dederick C. Ward
Publisher: Geological Society of America
ISBN: 0813721431
Category : Dissertations, Academic
Languages : en
Pages : 449
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Book Description
Author: Karen L. Kleinspehn
Publisher: Springer Science & Business Media
ISBN: 1461237882
Category : Science
Languages : en
Pages : 463
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Book Description
In the extensive field of earth sciences, with its many subdisciplines, the trans fer of knowledge is primarily established via personal communication, during meetings, by reading journal articles, or by consulting books. Because more information is available than can be assimilated, it is necessary for the individual to search selectively. Books take more time from the inception of an idea until publication than any of the other means of communication men tioned. As a consequence, their function is somewhat different. Many good books are a compilation of up to date knowledge and serve as reference or instruction manuals. Some books are a collection of previously published papers dealing with a certain topic, while others may basically provide large sets of data or examples. The Frontiers in Sedimentary Geology series was established both for stu dents and practicing earth scientists who wish to either stay abreast of the most recent ideas or developments or to become familiar with an important topic in the field of sedimentary geology. The series attempts to deal with sub jects that are in the forefront of both scientific and economic interest. The treatment of a subject in an individual volume should be a combination of topi cal, regional, and interdisciplinary approaches. Although these three terms can be defined separately, in reality they should flow into each other. A topical treatment should relate to a major category of sedimentary geology.
Author: Paul Kibler Sims
Publisher:
ISBN:
Category : Faults (Geology)
Languages : en
Pages : 268
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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.
