Continent formation through time-Reference-Cited by-同舟云学术

Continent formation through time

Published:2014-11-13 Issue:1 Volume:389 Page:1-16
ISSN:0305-8719
Container-title:Geological Society, London, Special Publications
language:en
Short-container-title:Geological Society, London, Special Publications

Author:

Roberts Nick M. W.¹,Van Kranendonk Martin J.²,Parman Stephen³,Clift Peter D.⁴

Affiliation:

1. NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK

2. School of Biological, Earth and Environmental Sciences, and Australian Centre for Astrobiology, University of New South Wales, Kensington, NSW 2052, Australia

3. Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, RI 02912, USA

4. Department of Geology and Geophysics, Louisiana State University, Baton Rouge, LA 70803, USA

Abstract

AbstractThe continental crust is the primary archive of geological history, and is host to most of our natural resources. Thus, the following remain critical questions in Earth Science, and provide an underlying theme to all of the contributions within this volume: when, how and where did the continental crust form? How did it differentiate and evolve through time? How has it has been preserved in the geological record? This introductory review provides a background to these themes, and provides an outline of the contributions contained within this volume.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference135 articles.

1. A model for the evolution of strontium and lead isotopes in a dynamic Earth

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5. Bastow I. D. Eaton D. W. (2013) in Continent Formation Through Time, The Hudson Bay Lithospheric Experiment (HuBLE): insights into Precambrian plate tectonics and the development of mantle keels, Geological Society, London, Special Publications, eds Roberts N. M. W. Van Kranendonk M. Parman S. Shirey S. Clift P. D. First published online November 27, 2013, http://dx.doi.org/10.1144/SP389.7 , 389.

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