Natural oxides, elements and remanent magnetization intensities and directions at DSDP Hole 93-603B@en
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Dark green spherules occur in the lower part of a turbidite in Section 603B-22-3, at the 70 cm level. In all probability these spherules originally consisted of massive glass, but now appear to have become completely altered into smectite. The presence of numerous microscopic fissures in the spherules probably mediated in the alteration process. […]
在603B-22-3剖面的浊积岩下部70厘米层位中，产出深绿色球状体。该类球状体最初极可能由块状玻璃质构成，但目前已完全蚀变为蒙脱石（smectite）。球状体中存在的大量显微裂隙，大概率在其蚀变过程中发挥了介导作用。[…]
创建时间：
2026-04-14
