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Archaean Geochemistry: The Origin and Evolution of the Archaean Continental Crus

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Category:

Books & Magazines

Quantity Available:

Only one in stock, order soon

Condition:

Used; Very Good

ISBN:

0387137467

EAN:

9780387137469

binding:

hardcover

format:

hardcover

language:

english

Externally Assigned Product Identifier:

0387137467

manufacturer:

Springer Verlag

author:

Gilbert N. Hanson

Publication Date:

1984-12-01T00:00:00Z

Subject Keyword:

'conservation', 'origin', 'evolution', 'geochemistry'

brand:

Springer Verlag

Product Site Launch Date:

2006-10-21T20:26:00-00:00

Part Number:

9780387137469

mpn:

9780387137469

ISBN-10:

0387137467

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Posted for sale:

More than a week ago

Item number:

1560322603

Item description

Ex-library from small college library - appears it was not checked out - usual library markings and envelop. Pages in good condition - writing on less than 10 pages in addition to library writing. Cover shows some of wear - scuffs along edges Buy with confidence because every order ships with delivery confirmation tracking number. Fast shipping from our non-smoking home. 2010AMA357 Additional Details ------------------------------ Product description: Archaean Geochemistry 1972 - 1984 The realisation that the continental crust contains well-preserved relics which date as far back as 4/5 of the Earth's age has given a great impetus to the study of early Precambrian terrains. As late as the mid-sixties the Archaean still constituted the 'terra-in cognita' of earth science. High metamorphic grades, poor out crop, and not least a widely assumed obliteration of early crustal records by convective recycling and thermal reworking had com bined to discourage research in this field. Many excellent local studies existed, notably around gold mining centres, but remained unrelated to a broader regional and theoretical understanding. This situation has changed as the consequence of two inter-related factors: (1) advances in isotopic methods and their application to Precambrian rocks, and (2) the recognition that some of the oldest terrains have retained a wealth of primary igneous and sedi mentary textures and even geochemical characteristics.