Abstract
Seamounts are features generated by hot spots and associated intraplate volcanic activity. The geochemical characteristics of igneous rocks constituting seamounts provide evidence of important details of dynamic processes in the Earth, such as mantle magma source areas, and are key to understanding how mantle plume processes control the formation and evolution of seamounts and their resulting geochemical characteristics. The Pacific Ocean contains a large number of hitherto unstudied seamounts, whose ages and geochemical characteristics remain poorly known. This study presents the geochemical characteristics of six basalt samples from five seamounts in the Western Pacific and the 40Ar/9Ar ages of three samples are determined. The new analysis yielded 40Ar/39Ar ages for seamounts samples MP3D21, MP5D11, and MP5D15A of 95.43 ± 0.33, 62.4 ± 0.26, and 99.03 ± 0.4 Ma, respectively. The geochemical profiles of seamounts samples MP3D04, MP3D21, MP5D11, MP5D15A, MPID201, and MPID202 are consistent with alkaline basalts, as evidence by alkali-rich, silicon-poor compositions along with high titanium concentrations. The primitive mantle normalized rare-earth elements and trace elements spider pattern are similar to those of ocean island basalts. The Ta/Hf and Nb/Zr ratios and La/Zr-Nb/Zr discriminant diagrams indicate that the six seamounts formed from magma that originated in the deep mantle.
Highlights
The close relationship between hot spot features and plate motion has long been a subject of intense academic research interest
The geochemical profiles of seamounts samples MP3D04, MP3D21, MP5D11, MP5D15A, MPID201, and MPID202 are consistent with alkaline basalts, as evidence by alkali-rich, silicon-poor compositions along with high titanium concentrations
We present the geochemical characterization of basalts from six seamounts in the Western Pacific, from which we selected three samples for Ar/ Ar dating
Summary
The close relationship between hot spot features and plate motion has long been a subject of intense academic research interest. Seamounts are usually described as underwater highlands more than 1000 m above the seabed. They are very common volcanic landforms on the Earth. Because seamounts record evidence of intraplate volcanic eruptions, they provide important information for understanding the nature of hot spot volcanic activity, and they have received high levels of research attention [4,5,6,7,8,9,10]. The geochemical characteristics of provide important information about dynamic processes in the Earth, such as mantle magma source areas, which are key to better understanding how mantle processes determine the formation and evolution of seamounts and their resulting geochemical characteristics [11,12,13,14,15,16,17,18,19]. Seamounts contain a large variety of materials that constitute valuable seabed resources, such as cobalt-rich crusts
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