Abundant hydrothermal venting along melt‐rich and melt‐free ridge segments in the Lau back‐arc basin
- 6 April 2006
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 33 (7)
- https://doi.org/10.1029/2005gl025283
Abstract
No abstract availableThis publication has 23 references indexed in Scilit:
- Opposing trends in crustal thickness and spreading rate along the back-arc Eastern Lau Spreading Center: Implications for controls on ridge morphology, faulting, and hydrothermal activityEarth and Planetary Science Letters, 2006
- Hydrothermal activity on near‐arc sections of back‐arc ridges: Results from the Mariana Trough and Lau BasinGeochemistry, Geophysics, Geosystems, 2005
- Hydrothermal venting along Earth's fastest spreading center: East Pacific Rise, 27.5°–32.3°Journal of Geophysical Research, 2002
- Mantle wedge control on back-arc crustal accretionNature, 2002
- Hydrothermal plumes along segments of contrasting magmatic influence, 15°20′–18°30′N, East Pacific Rise: Influence of axial faultingGeochemistry, Geophysics, Geosystems, 2001
- A three‐plate kinematic model for Lau Basin openingGeochemistry, Geophysics, Geosystems, 2001
- The January 1998 Earthquake swarm at Axial Volcano, Juan de Fuca Ridge: Hydroacoustic evidence of seafloor volcanic activityGeophysical Research Letters, 1999
- Seismic structure and indicators of magma budget along the Southern East Pacific RiseJournal of Geophysical Research, 1997
- Hydrothermal plumes along the East Pacific Rise, 8°40′ to 11°50′N: Plume distribution and relationship to the apparent magmatic budgetEarth and Planetary Science Letters, 1994
- Seismic Structure of the Southern East Pacific RiseScience, 1993