The RAMESSES experiment-II. Evidence for accumulated melt beneath a slow spreading ridge from wide-angle refraction and multichannel reflection seismic profiles-Reference-Cited by-同舟云学术

The RAMESSES experiment-II. Evidence for accumulated melt beneath a slow spreading ridge from wide-angle refraction and multichannel reflection seismic profiles

Published:1998-12 Issue:3 Volume:135 Page:746-772
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Navin D. A.,Peirce C.,Sinha M. C.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/135/3/746/1730537/135-3-746.pdf

Reference60 articles.

1. Structure and variability of oceanic crust on the flanks of the East Pacific Rise between 11° and 13°N;Bratt;J. geophys. Res.,1984

2. Seismic evidence for a magma chamber beneath the slow-spreading Mid-Atlantic Ridge;Calvert;Nature,1995

3. Tomographic image of the axial low velocity zone at 12°50′N on the East Pacific Rise;Caress;J. geophys. Res.,1992

4. Density of the oceanic crust;Carlson;Nature,1984

5. Body-wave seismograms in inhomogeneous media using Maslov asymptotic theory;Chapman;Bull. seism. Soc. Am.,1982

Cited by 75 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Beyond spreading rate: Controls on the thermal regime of mid-ocean ridges;Proceedings of the National Academy of Sciences;2023-10-30

2. Magma source region size controls along axis variations in crustal thickness, axial depth and relief at plate spreading centers;Earth and Planetary Science Letters;2021-12

3. Global Trends of Axial Relief and Faulting at Plate Spreading Centers Imply Discrete Magmatic Events;Journal of Geophysical Research: Solid Earth;2020-07-31

4. Zoned Crystal Records of Transcrustal Magma Transport, Storage and Differentiation: Insights from the Shatsky Rise Oceanic Plateau;Journal of Petrology;2020-07-24

5. On spreading rates and crustal structure at mid-ocean ridges;CHINESE J GEOPHYS-CH;2020