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(Table 1) Mineralogy of sediments at DSDP Site 61-462
Two holes (462, 462A) were drilled at Site 462 in the Nauru Basin, within an area formed at a fast-spreading Pacific-plate boundary 145 to 155 m.y. ago. Forty-eight sediment... -
(Table T1) Physical properties of minicores from ODP Leg 193 sites, PACMANUS ...
Permeability of the ocean crust is one of the most crucial parameters for constraining submarine fluid flow systems. Active hydrothermal fields are dynamic areas where fluid... -
X-ray diffraction analysis of sediments from ODP Hole 178-1095B
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Mineral composition of bulk sediment from Hole 7-61A
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Mineral composition of bulk sediment from Hole 6-52
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Effects of Local Displacements on Phase Transitions in Sr- and Ca-substituted...
Ferroelectric BaTiO3 (BT) constitutes a base system for many practical applications ranging from classical capacitors to tunable dielectrics. A dielectric response in BT is... -
Mineralogy of nonclay components of Hole 325-M0058A
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