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Tectonic response of the central Chilean margin (35-38°S) to the collision and subduction of heterogeneous oceanic crust : a thermochronological study

Author
SPIKINGS, R1 ; DUNGAN, M1 ; FOEKEN, J2 ; CARTER, A3 ; PAGE, L4 ; STUART, F2
[1] Department of Mineralogy, University of Geneva, 13 Rue des Maraichers, Geneva 1205, Switzerland
[2] Scottish Universities Environmental Research Centre, Rankine Avenue, Scottish Enterprise Technology Park, East Kilbride G75 0QF, United Kingdom
[3] School of Earth Sciences, Birkbeck College, Malet Street, London WC1E 7HX, United Kingdom
[4] Department of Geology, GeoBiosphere Science Centre, Lund University, Solvegatan 12, 223 62 Lund, Sweden
Source

Journal of the Geological Society (London). 2008, Vol 165, pp 941-953, 13 p ; 5 ; ref : 1 p.1/4

CODEN
JGSLAS
ISSN
0016-7649
Scientific domain
Geology; Geophysics
Publisher
Geological Society, London
Publication country
United Kingdom
Document type
Article
Language
English
Keyword (fr)
Apatite Aplatissement Climat Cordillère Croûte océanique Dalle Durée Exhumation Intrusion Ligne directionnelle Plaque Sud Américaine Refroidissement Résistance mécanique Segmentation Subduction Tectonique Topographie Trace fission Zircon Chili Nésosilicate Phosphate Silicate Amérique du Sud
Keyword (en)
apatite flattening climate Cordillera oceanic crust slabs duration exhumation intrusions strike South American Plate cooling strength segmentation subduction tectonics topography fission tracks zircon Chile nesosilicates phosphates silicates South America
Keyword (es)
Apatito Clima Cordillera Corteza oceánica Losa Intrusión Enfriamiento Resistencia mecánica Subducción Tectónico Topografía Traza fisión Zircón Chile Fosfato Silicato America del sur
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01F Crystalline rocks / 001E01F01 Igneous and metamorphic rocks petrology, volcanic processes, magmas

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
20603209

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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