Steady and non-steady state magma chambers below the East Pacific Rise-Reference-Cited by-同舟云学术

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Steady and non-steady state magma chambers below the East Pacific Rise

Published:1996-02-01 Issue:3 Volume:23 Page:221-224
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Batiza Rodey,Niu Y.,Karsten J. L.,Boger W.,Potts E.,Norby L.,Butler R.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/v023/i003/95GL00016/95GL00016.pdf

Reference24 articles.

1. The Mid-Atlantic Ridge near 45°N, II. Basalts from the area of Confederation Peak;Aumento;Can. J. Earth Sci.,1968

2. The origin of bathymetric highs at ridge-transform intersections: A multi-disciplinary case study at the Clipperton Fracture Zone;Barth;Mar. Geophys. Res.,1994

3. Petrology and magma chamber processes at the East Pacific Rise ˜9°30′N;Batiza;J. Geophys. Res.,1992

4. Petrogenesis of basalts from the project FAMOUS area: experimental study from 0 to 15 kbars;Bender;Earth Planet. Sci. Lett.,1978

5. East Pacific Rise 8°-10°30′N: evolution of ridge segments and discontinuities from SeaMARC II and three-dimensional magnetic studies;Carbotte;J. Geophys. Res.,1992

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1. Copper isotope fractionation during magma differentiation: Evidence from lavas on the East Pacific Rise at 10°30′N;Geochimica et Cosmochimica Acta;2023-09

2. Zinc isotope fractionation during mid-ocean ridge basalt differentiation: Evidence from lavas on the East Pacific Rise at 10°30′N;Geochimica et Cosmochimica Acta;2023-04

3. Molybdenum isotope systematics of lavas from the East Pacific Rise: Constraints on the source of enriched mid-ocean ridge basalt;Earth and Planetary Science Letters;2022-01

4. High‐Resolution Isotopic Variability Across EPR Segment 16°N: A Chronological Interpretation of Source Composition and Ridge‐Seamount Interaction;Geochemistry, Geophysics, Geosystems;2021-10

5. Extreme Heterogeneity in Mid‐Ocean Ridge Mantle Revealed in Lavas From the 8°20′N Near‐Axis Seamount Chain;Geochemistry, Geophysics, Geosystems;2021-01

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