Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt

This article aims to provide a simple and applicable method of measuring the rock accumulation rate and recording the depositional events based on the application of graphic correlation and similarity matrix of the Paleogene planktonic foraminifera in two surface sections in South Sinai. Fifteen con...

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Published in:Geological Journal
Main Authors: Hassan, Hatem F., Al‐Helal, Anwar B., Platon, Emil
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1002/gj.4702
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spelling crwiley:10.1002/gj.4702 2024-06-02T08:13:26+00:00 Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt Hassan, Hatem F. Al‐Helal, Anwar B. Platon, Emil 2023 http://dx.doi.org/10.1002/gj.4702 https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4702 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/gj.4702 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Geological Journal volume 58, issue 5, page 1965-1989 ISSN 0072-1050 1099-1034 journal-article 2023 crwiley https://doi.org/10.1002/gj.4702 2024-05-03T10:44:41Z This article aims to provide a simple and applicable method of measuring the rock accumulation rate and recording the depositional events based on the application of graphic correlation and similarity matrix of the Paleogene planktonic foraminifera in two surface sections in South Sinai. Fifteen continuous biozones and subzones were recorded spanning from P0 to E3. The average RAR of the Beida Formation was somewhat equal to that recorded for the Dakhla Formation, however, the Selandian‐Ypresian Garra Formation was more than twice that recorded for the Esna Formation. On the other hand, the Thebes Formation represents a reverse setting which is relatively higher in the south than the north. Seven (T1‐T7) and twelve (T1‐T12) terraces were recorded at different stratigraphic positions. The terraces diverged in the Palaeocene and converged in the Eocene, whereas they lengthen in the Palaeocene and shortened in the Eocene. Breaks identified in the SM support many of the poorly constrained terraces on the GC, however, the SM technique efficiently recorded around 60% of the terraces recorded by GC. For confirming the terraces identified, field and faunal parameters confirm all the recorded events, however, a further correlation with their equivalent in and outside Egypt has been made which confirms another support of the technique applied. Therefore, the integration between these techniques in recognizing the depositional events and sedimentation breaks supports further depositional and palaeobathymetical studies and regional correlation as well. Article in Journal/Newspaper Planktonic foraminifera Wiley Online Library Geological Journal 58 5 1965 1989
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description This article aims to provide a simple and applicable method of measuring the rock accumulation rate and recording the depositional events based on the application of graphic correlation and similarity matrix of the Paleogene planktonic foraminifera in two surface sections in South Sinai. Fifteen continuous biozones and subzones were recorded spanning from P0 to E3. The average RAR of the Beida Formation was somewhat equal to that recorded for the Dakhla Formation, however, the Selandian‐Ypresian Garra Formation was more than twice that recorded for the Esna Formation. On the other hand, the Thebes Formation represents a reverse setting which is relatively higher in the south than the north. Seven (T1‐T7) and twelve (T1‐T12) terraces were recorded at different stratigraphic positions. The terraces diverged in the Palaeocene and converged in the Eocene, whereas they lengthen in the Palaeocene and shortened in the Eocene. Breaks identified in the SM support many of the poorly constrained terraces on the GC, however, the SM technique efficiently recorded around 60% of the terraces recorded by GC. For confirming the terraces identified, field and faunal parameters confirm all the recorded events, however, a further correlation with their equivalent in and outside Egypt has been made which confirms another support of the technique applied. Therefore, the integration between these techniques in recognizing the depositional events and sedimentation breaks supports further depositional and palaeobathymetical studies and regional correlation as well.
format Article in Journal/Newspaper
author Hassan, Hatem F.
Al‐Helal, Anwar B.
Platon, Emil
spellingShingle Hassan, Hatem F.
Al‐Helal, Anwar B.
Platon, Emil
Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt
author_facet Hassan, Hatem F.
Al‐Helal, Anwar B.
Platon, Emil
author_sort Hassan, Hatem F.
title Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt
title_short Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt
title_full Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt
title_fullStr Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt
title_full_unstemmed Integrating graphic correlation and similarity matrix of the Early Paleogene rock units in South Sinai, Egypt
title_sort integrating graphic correlation and similarity matrix of the early paleogene rock units in south sinai, egypt
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1002/gj.4702
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4702
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/gj.4702
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Geological Journal
volume 58, issue 5, page 1965-1989
ISSN 0072-1050 1099-1034
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/gj.4702
container_title Geological Journal
container_volume 58
container_issue 5
container_start_page 1965
op_container_end_page 1989
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