Annotated record of the detailed examination of Mn deposits from the Aotea Se...
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An elongate ENE-trending seamount in the New Caledonia Basin is interpreted as the product of basaltic fissure eruption. The age is unknown, but Pleistocene-Recent shallow water...
新喀里多尼亚海盆(New Caledonia Basin)内一座呈东东北(ENE)走向的狭长海山(seamount),被解释为玄武岩裂隙喷发(basaltic fissure eruption)作用的产物。其形成年代尚不明确,但该区域存在更新世(Pleistocene)-近代的浅水环境……



