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Geochemical evolution of Earth's con...
~
Keller, C. Brenhin.
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Geochemical evolution of Earth's continental crust.
Record Type:
Electronic resources : Monograph/item
Title/Author:
Geochemical evolution of Earth's continental crust./
Author:
Keller, C. Brenhin.
Published:
Ann Arbor : ProQuest Dissertations & Theses, : 2016,
Description:
184 p.
Notes:
Source: Dissertation Abstracts International, Volume: 78-05(E), Section: B.
Contained By:
Dissertation Abstracts International78-05B(E).
Subject:
Geochemistry. -
Online resource:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10195599
ISBN:
9781369377934
Geochemical evolution of Earth's continental crust.
Keller, C. Brenhin.
Geochemical evolution of Earth's continental crust.
- Ann Arbor : ProQuest Dissertations & Theses, 2016 - 184 p.
Source: Dissertation Abstracts International, Volume: 78-05(E), Section: B.
Thesis (Ph.D.)--Princeton University, 2016.
This item is not available from ProQuest Dissertations & Theses.
Earth's unique continental crust represents the active interface between the deep earth and the surface earth system, and is crucial for the survival and diversification of life on Earth, both as a source for nutrients and a component in the silicate weathering feedback that stabilizes Earth's equable climate on billion-year timescales. However, many open questions remain regarding the formation and secular temporal evolution of Earth's crust -- in part due to the extremely poorly-mixed nature of Earth's continental crust such that compositional heterogeneity at any one point in geologic time typically dwarfs any systematic variation over time. New computational approaches enabled by the emergence of large, freely accessible geochemical datasets provide a way to see through this heterogeneity and extract quantitative information about underlying processes and variables that drive the evolution of Earth's crust over geologic time.
ISBN: 9781369377934Subjects--Topical Terms:
539092
Geochemistry.
Geochemical evolution of Earth's continental crust.
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Earth's unique continental crust represents the active interface between the deep earth and the surface earth system, and is crucial for the survival and diversification of life on Earth, both as a source for nutrients and a component in the silicate weathering feedback that stabilizes Earth's equable climate on billion-year timescales. However, many open questions remain regarding the formation and secular temporal evolution of Earth's crust -- in part due to the extremely poorly-mixed nature of Earth's continental crust such that compositional heterogeneity at any one point in geologic time typically dwarfs any systematic variation over time. New computational approaches enabled by the emergence of large, freely accessible geochemical datasets provide a way to see through this heterogeneity and extract quantitative information about underlying processes and variables that drive the evolution of Earth's crust over geologic time.
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http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10195599
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