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The cores are composed of diatom-bearing, olive-gray, silty clay.
Furthermore, the liquefied breccia segment cores are composed of gray sandstone and black siltstone, which may be seismites resulting from intense and strong earthquakes during the late Triassic.
The resulting cisplatin cores are composed entirely of cisplatin and stabilized by DOPA with a drug loading of approximately 93 wt % and have tunable sizes between 12 and 75 nm.
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The light biocrust cores were composed of 95% light cyanobacterial crust cover and only 3% dark crust cover.
The cores were composed of high- and low-density balsa layers separated by a circular adhesive interface or FRP arch.
The Takanoobane rhyolite lava in the two cores is composed of an inner crystalline part, and marginal glassy parts (upper and basal glassy layers) (Furukawa and Kamata, 2005; Furukawa et al., 2010) (Fig. 1(c)).
The sediments in the core are composed of six major units which can be further divided into subunits.
This is reasonable considering that albedo and vascular core are composed of a colorless, spongy network of parenchymatous cells.
All experimental long core is composed by eleven short cores.
The inner core is composed by several nuclei of around 4 nm diameter.
The core is composed of alternating layers of silty-claystone and claystone.
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