Sedimentalogical Evolution of the northern Baer-Bassit during upper Cretaceous

Authors

  • Abdulkarim AlAbdalla Tishreen university
  • Samer AL-BUB Tishreen University

Abstract

The sedimentological study of five geological sections in the Upper Cretaceous deposits, exposed in northern Al-Baer-Basit which located beneath the ophiolitic cover, revealed the presence of four intermediate sedimentary sequences in the Turonian-Senonian deposits: regressive, transgressive-neutral, regressive-regressive and transgressive. These sedimentary sequences are related to sea level changes and the uplift of the bottom of the sedimentary basin because of ophiolitic obduction in northwestern of Syria. During the Turonian-Senonian, the sedimentation environments ranged from subtidal in the open sea to supratidal to even continental environments, in which sediments are rich in detrital were dominant

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Published

2024-04-23

How to Cite

1.
العبد الله عا, سامر البب. Sedimentalogical Evolution of the northern Baer-Bassit during upper Cretaceous. TUJ-BA [Internet]. 2024Apr.23 [cited 2024Nov.24];46(1):25-46. Available from: https://journal.tishreen.edu.sy/index.php/bassnc/article/view/16225

Issue

Vol. 46 No. 1 (2024): Tishreen University Journal of Research and Scientific Studies - Basic Sciences Series

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