The Line Islands volcanic chain in the central Pacific Ocean exhibits many characteristics of a hotspot-generated seamount chain; however, the lack of a predictable age progression has stymied previous models for the origin of this feature. We combined plate-tectonic reconstructions with seamount age dates and available geochemistry to develop a new model that involves multiple melt regions and multiple melt delivery styles to explain the spatial and temporal history of the Line Islands system. Our model identifies a new melt source region (Larson melt region at ~17°S, ~125°W) that contributed to the formation of the Line Islands, as well as the Mid-Pacific Mountains and possibly the Pukapuka Ridge.
|Publication Subtype||Journal Article|
|Title||Multiple melt source origin of the Line Islands (Pacific Ocean)|
|Publisher||Geological Society of America|
|Contributing office(s)||Pacific Coastal and Marine Science Center|
|Other Geospatial||Line Islands|
|Google Analytic Metrics||Metrics page|