Document Type

Article

Date of Original Version

11-1-2021

Abstract

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 Title, e.g., Journal

Geology

Volume

49

Issue

11

Creative Commons License

Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.

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