Abstract
Detailed lithologic, microfaunal, and biometric investigations, using relative abundances, diversity indexes, and duration charts of ostracods and foraminifera, allowed the recognition of sea level changes during the Cretaceous of Israel. Four anoxic events (black shales) accompanying transgressions correspond to the Cretaceous oceanic record. We hypothesize the presence of mature oil shales in the present-day eastern Mediterranean basin close to allochthonous reef blocks detached from the Cretaceous platform.
Original language | English |
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Pages (from-to) | 1685-1699 |
Number of pages | 15 |
Journal | AAPG Bulletin |
Volume | 70 |
Issue number | 11 |
State | Published - Nov 1986 |