Plagioclase preferred orientation and induced seismic anisotropy in mafic igneous rocks-Reference-Cited by-同舟云学术

Plagioclase preferred orientation and induced seismic anisotropy in mafic igneous rocks

Published:2014-11 Issue:11 Volume:119 Page:8064-8088
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Ji Shaocheng¹,Shao Tongbin¹,Salisbury Matthew H.²,Sun Shengsi³,Michibayashi Katsuyoshi⁴,Zhao Weihua⁵,Long Changxing⁵,Liang Fenghua⁶,Satsukawa Takako⁷

Affiliation:

1. Département des Génies Civil, Géologique et des Mines; École Polytechnique de Montréal; Montréal Québec Canada

2. Geological Survey of Canada-Atlantic; Bedford Institute of Oceanography; Halifax Nova Scotia Canada

3. State Key Laboratory of Continental Dynamics, Department of Geology; Northwest University; Xi'an Shangxi China

4. Department of Geosciences, Faculty of Science; Shizuoka University; Shizuoka Japan

5. Institute of Geomechanics; Chinese Academy of Geological Sciences; Beijing China

6. State Key Laboratory for Continental Tectonics and Dynamics, Institute of Geology; Chinese Academy of Geological Sciences; Beijing China

7. ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) & GEMOC; Department of Earth and Planetary Sciences; Macquarie University; Sydney New South Wales Australia

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JB011352/fullpdf

Reference125 articles.

1. Deformation microstructures and lattice orientations of plagioclase in gabbros from Central Australia;Ague;Geophys. Monogr.,1990

2. Velocities of elastic waves in minerals at atmospheric pressure and increasing precision of elastic constants by means of EVM [in Russian];Aleksandrov;Izv. Acad. Sci. USSR, Geol. Ser.,1974

3. Anorthosites

4. Barruol , G. 1993 Pétrophysique de la croûte inférieure

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