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 Lower Cretaceous sediments in Jordan consist mostly of sandstone with intercalations of claystones of deltaic and fluviatile origin, in addition to marine carbonate interbeds (Fayez and Hakam, 1994). Abed (1978, 1982) described the sandstones in North Jordan in general as varicolored, friable, quartz-arenitic sandstone attains a thickness of 300 m. He postulated that these sandstones are of fluvial origin with a few interfingering shallow marine horizons. Abed (1982) reported rich fern-like macroflora from the siltstone facies at Kurnub locality in North Jordan. The present study is an attempt to clarify the stratigraphical position and partially depositional conditions of Kurnub Sandstone (Fig. 1) by studying its macro and microfloral content.

Plant Impressions and Sporomorphs from Kurnub Sandstone Formation in North Jordan