(Table 2) Oxygen isotopic composition and calculated temperatures of formation of clay minerals from DSDP Hole 504B@en
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Depth, sediment (m) is the sub-basement depth (m), Sample 70-504B-37-1,76-80 calculated after Yeh and Savin (1977, doi:10.1130/0016-7606(1977)88<1321:MOBMOA>2.0.CO;2), sample 83-405B-80-1,106-111 calculated T = 200-250 °C calculated after Wenner and Taylor (1971, doi:10.1007/BF00643332)
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2026-04-24
