Late Cretaceous evolution of the Judean Mountains as indicated by ostracodes

A. Flexer; A. Gilat; F. Hirsch; A. Honigstein; A. Rosenfeld; T. Rueffer

doi:10.1111/j.1365-3121.1989.tb00385.x

Late Cretaceous evolution of the Judean Mountains as indicated by ostracodes

A. Flexer^*, A. Gilat, F. Hirsch, A. Honigstein, A. Rosenfeld, T. Rueffer

^*Corresponding author for this work

School of the Environment and Earth Sciences

Research output: Contribution to journal › Article › peer-review

17 Scopus citations

Abstract

The Judean Mountains’ anticlinorium, Israel, a part of the Syrian Arc fold system, underwent several phases of compressional folding, uplift and faulting in post‐Turonian through Quaternary times. This study emphasizes the earliest tectonic phase of earIy Late Coniacian age. Ostracode biozonation clearly indicates the duration and extension of Senonian sedimentation and timing of onlap over the evolving Judean Mountains’ structure.

Original language	English
Pages (from-to)	349-358
Number of pages	10
Journal	Terra Nova
Volume	1
Issue number	4
DOIs	https://doi.org/10.1111/j.1365-3121.1989.tb00385.x
State	Published - Jul 1989

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10.1111/j.1365-3121.1989.tb00385.x

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Late Cretaceous evolution of the Judean Mountains as indicated by ostracodes

Abstract

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