A lithospheric perspective on structure and evolution of Precambrian cratons

Publikation: Bidrag til bog/antologi/rapport › Bidrag til bog/antologi › Forskning › fagfællebedømt

Standard

A lithospheric perspective on structure and evolution of Precambrian cratons. / Artemieva, Irina.

Regional geology and tectonics: principles of geologic analysis. red. / D.G. Roberts; A.W. Bally. Elsevier, 2012. s. 95-111.

Publikation: Bidrag til bog/antologi/rapport › Bidrag til bog/antologi › Forskning › fagfællebedømt

Harvard

Artemieva, I 2012, A lithospheric perspective on structure and evolution of Precambrian cratons. i DG Roberts & AW Bally (red), Regional geology and tectonics: principles of geologic analysis. Elsevier, s. 95-111.

APA

Artemieva, I. (2012). A lithospheric perspective on structure and evolution of Precambrian cratons. I D. G. Roberts, & A. W. Bally (red.), Regional geology and tectonics: principles of geologic analysis (s. 95-111). Elsevier.

Vancouver

Artemieva I. A lithospheric perspective on structure and evolution of Precambrian cratons. I Roberts DG, Bally AW, red., Regional geology and tectonics: principles of geologic analysis. Elsevier. 2012. s. 95-111

Author

Artemieva, Irina. / A lithospheric perspective on structure and evolution of Precambrian cratons. Regional geology and tectonics: principles of geologic analysis. red. / D.G. Roberts ; A.W. Bally. Elsevier, 2012. s. 95-111

Bibtex

@inbook{e2d16da0ba0d11ddae57000ea68e967b,
title = "A lithospheric perspective on structure and evolution of Precambrian cratons",
abstract = "The purpose of this chapter is to provide a summary of geophysical data on thestructure of the stable continental lithosphere and its evolution since theArchean. Here, the term lithosphere is used to define the outer layer of the Earthwhich includes the crust and uppermost mantle, forms the roots of the continents,and moves together with continental plates. Depending on geophysicaltechniques (and physical properties measured), the lithosphere has differentpractical definitions. Most of them (i.e., seismic, electrical) are on the basis of asharp change in temperature-dependent physical properties at the transitionfrom conductive to convecting mantle.",
author = "Irina Artemieva",
year = "2012",
language = "English",
isbn = "978-0-444-53042-4",
pages = "95--111",
editor = "D.G. Roberts and A.W. Bally",
booktitle = "Regional geology and tectonics",
publisher = "Elsevier",
address = "Netherlands",

}

RIS

TY - CHAP

T1 - A lithospheric perspective on structure and evolution of Precambrian cratons

AU - Artemieva, Irina

PY - 2012

Y1 - 2012

N2 - The purpose of this chapter is to provide a summary of geophysical data on thestructure of the stable continental lithosphere and its evolution since theArchean. Here, the term lithosphere is used to define the outer layer of the Earthwhich includes the crust and uppermost mantle, forms the roots of the continents,and moves together with continental plates. Depending on geophysicaltechniques (and physical properties measured), the lithosphere has differentpractical definitions. Most of them (i.e., seismic, electrical) are on the basis of asharp change in temperature-dependent physical properties at the transitionfrom conductive to convecting mantle.

AB - The purpose of this chapter is to provide a summary of geophysical data on thestructure of the stable continental lithosphere and its evolution since theArchean. Here, the term lithosphere is used to define the outer layer of the Earthwhich includes the crust and uppermost mantle, forms the roots of the continents,and moves together with continental plates. Depending on geophysicaltechniques (and physical properties measured), the lithosphere has differentpractical definitions. Most of them (i.e., seismic, electrical) are on the basis of asharp change in temperature-dependent physical properties at the transitionfrom conductive to convecting mantle.

M3 - Book chapter

SN - 978-0-444-53042-4

SP - 95

EP - 111

BT - Regional geology and tectonics

A2 - Roberts, D.G.

A2 - Bally, A.W.

PB - Elsevier

ER -

ID: 8743608