English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

The present investigation deals with the lithostratigraphy and planktonic foraminiferal biostatigraphy of the Shiranish Formation from a surface section in Sinjar area, جن سراف و يلوتملا يدجم دجام يروبجلا سر 153 northwestern Iraq. Depending on lithological characteristic, the formation is divided into three units: the lower unit consists of friable marl, the middle unit embrace an alternations of marl, marly limestone, limestone, sandy limestone and lenses of breccia, while the upper unit is consist of marl and marly limestone. The stratigraphic distribution of the planktonic foraminifera throughout the section permits the recognition of four zones, these are: 1. Globotruncanita calcarata Zone. 2. Globotruncanella havanensis – Rosita fornicata Zone. 3. Globotruncana aegyptiaca Zone. 4. Gansserina gansseri Zone, The present work indicates that Shiranish Formation is of Late Campanian-Late Maastrichtian age.

Litho and Biostratigraphy of the Shiranish Formation (Late Campanian-Late Maastrichtian) In Sinjar Area, Northwestern Iraq