Magma flow directions in the sheeted dike complex at superfast spreading mid-ocean ridges: Insights from IODP Hole 1256D, Eastern Pacific-Reference-Cited by-同舟云学术

Magma flow directions in the sheeted dike complex at superfast spreading mid-ocean ridges: Insights from IODP Hole 1256D, Eastern Pacific

Published:2014-04 Issue:4 Volume:15 Page:1283-1295
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Veloso Eugenio E.¹,Hayman Nicholas W.²,Anma Ryo³,Tominaga Masako⁴,González Rodrigo T.⁵,Yamazaki Toshitsugu⁶,Astudillo Natalia⁷

Affiliation:

1. Dirección de Investigaciones Científicas y Tecnológicas; Pontificia Universidad Católica de Chile; Avenida Vicuña Mackenna 4860 Santiago Chile 7820436

2. Institute for Geophysics; University of Texas; J.J. Pickle Research Campus; Austin Texas USA

3. Graduate School of Life and Environmental Sciences; University of Tsukuba; Tsukuba Japan

4. Department of Geological Sciences; Michigan State University; East Lansing Michigan USA

5. Facultad de Ingeniería y Ciencias Geológicas; Departamento de Ciencias Geológicas; Universidad Católica del Norte; Antofagasta Chile

6. Atmosphere and Ocean Research Institute; University of Tokyo; Kashiwa Japan

7. Servicio Nacional de Geología y Minería; Santiago Chile

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference52 articles.

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2. Magma flow in sub-aqueous rhyolitic dikes inferred from magnetic fabric analysis (Ponza Island, W. Italy);Aubourg;Phys. Chem. Earth,2002

3. Interpreting anomalous fabrics in ophiolite dikes;Borradaile;J. Struct. Geol.,2003

4. Tectonic stress and magma chamber size as control on dike propagation: Constraints from the 1975-1984 Krafla rifting episode;Buck;J. Geophys. Res.,2006

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