Many Archean and Proterozoic greenstone belts contain volcanic rocks that e
rupted subaqueously but interacted with continental crust on their way to t
he surface. This points to emplacement in a tectonic setting that was rare
to absent throughout the Phanerozoic - the eruption of flood basalts onto s
ubmerged continental platforms. To explain the situation requires that sea
levels were high during periods of flood volcanism, perhaps because the oce
an basins were partially filled by extensive, active and high-standing ocea
nic ridges or by oceanic plateaus. The common preservation of crust-contami
nated submarine basalts, even in the oldest supracrustal sequences, may ind
icate that continental crust was voluminous even at an early stage in Earth
history. (C) 1999 Elsevier Science B.V. All rights reserved.