Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia

The Crocker Formation, Late Eocene to Middle Miocene in age, was deposited in a deep-marine environment by a turbidity current. Most of the facies identified in the field are related to the sedimentary bed-form structures belonging to Bouma sequences. These prominently include unit divisions such as...

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Main Authors: Muhd Nur Ismail Abdul Rahman, Hafeez Jeofry, Muhammad Abdullah, Ismail Abd Rahim, Sanudin Hj.Tahir
Format: Article
Language:English
English
Published: Persatuan Geologi Malaysia 2021
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Online Access:https://eprints.ums.edu.my/id/eprint/31870/2/Facies%20analysis%20of%20the%20Late%20Eocene%20deep-marine%20middle-%20to%20outer-fan%20sequence%20of%20the%20Crocker%20Formation%20in%20Tenom%20District%2C%20Sabah%2C%20Malaysia_ABSTRACT.pdf
https://eprints.ums.edu.my/id/eprint/31870/1/Facies%20analysis%20of%20the%20Late%20Eocene%20deep-marine%20middle-%20to%20outer-fan%20sequence%20of%20the%20Crocker%20Formation%20in%20Tenom%20District%2C%20Sabah%2C%20Malaysia.pdf
https://eprints.ums.edu.my/id/eprint/31870/
https://gsm.org.my/products/702001-101922-PDF.pdf
http://dx.doi.org/10.7186/bgsm72202105
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spelling my.ums.eprints.318702022-03-16T08:30:39Z https://eprints.ums.edu.my/id/eprint/31870/ Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia Muhd Nur Ismail Abdul Rahman Hafeez Jeofry Muhammad Abdullah Ismail Abd Rahim Sanudin Hj.Tahir QE1-996.5 Geology The Crocker Formation, Late Eocene to Middle Miocene in age, was deposited in a deep-marine environment by a turbidity current. Most of the facies identified in the field are related to the sedimentary bed-form structures belonging to Bouma sequences. These prominently include unit divisions such as Ta referring to grading sand, Tb for parallel laminae, Tc for cross laminae, Td for mud laminae, and Te referring to hemipelagic mud. Five facies have adequately been identified using Bouma sequence implications, namely Facies 1 (F1: Ta-Tb layers), Facies 2 (F2: Ta-Te layers), Facies 3 (F3: Tb-Te layers), Facies 4 (F4: Tb / Tc-Te layers), and Facies 5 (F5: Td-Te layers). Based on the Crocker Formation facies analysis, three distinct groups of facies associations were recognised: Deep-Marine Channel-Lobe Association (Type A1), Deep-Marine Channel-Levee Association (Type A2), and Distal Lobe Association. These facies associations precisely revealed that the Crocker Formation's depositional environments were likely deposited in the middle-fan with associated outer-fan settings. Persatuan Geologi Malaysia 2021 Article PeerReviewed text en https://eprints.ums.edu.my/id/eprint/31870/2/Facies%20analysis%20of%20the%20Late%20Eocene%20deep-marine%20middle-%20to%20outer-fan%20sequence%20of%20the%20Crocker%20Formation%20in%20Tenom%20District%2C%20Sabah%2C%20Malaysia_ABSTRACT.pdf text en https://eprints.ums.edu.my/id/eprint/31870/1/Facies%20analysis%20of%20the%20Late%20Eocene%20deep-marine%20middle-%20to%20outer-fan%20sequence%20of%20the%20Crocker%20Formation%20in%20Tenom%20District%2C%20Sabah%2C%20Malaysia.pdf Muhd Nur Ismail Abdul Rahman and Hafeez Jeofry and Muhammad Abdullah and Ismail Abd Rahim and Sanudin Hj.Tahir (2021) Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia. Bulletin of the Geological Society of Malaysia, 72. pp. 47-62. ISSN 0126-6187 (P-ISSN) , 2637-109X (E-ISSN) https://gsm.org.my/products/702001-101922-PDF.pdf http://dx.doi.org/10.7186/bgsm72202105
institution Universiti Malaysia Sabah
building UMS Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Sabah
content_source UMS Institutional Repository
url_provider http://eprints.ums.edu.my/
language English
English
topic QE1-996.5 Geology
spellingShingle QE1-996.5 Geology
Muhd Nur Ismail Abdul Rahman
Hafeez Jeofry
Muhammad Abdullah
Ismail Abd Rahim
Sanudin Hj.Tahir
Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia
description The Crocker Formation, Late Eocene to Middle Miocene in age, was deposited in a deep-marine environment by a turbidity current. Most of the facies identified in the field are related to the sedimentary bed-form structures belonging to Bouma sequences. These prominently include unit divisions such as Ta referring to grading sand, Tb for parallel laminae, Tc for cross laminae, Td for mud laminae, and Te referring to hemipelagic mud. Five facies have adequately been identified using Bouma sequence implications, namely Facies 1 (F1: Ta-Tb layers), Facies 2 (F2: Ta-Te layers), Facies 3 (F3: Tb-Te layers), Facies 4 (F4: Tb / Tc-Te layers), and Facies 5 (F5: Td-Te layers). Based on the Crocker Formation facies analysis, three distinct groups of facies associations were recognised: Deep-Marine Channel-Lobe Association (Type A1), Deep-Marine Channel-Levee Association (Type A2), and Distal Lobe Association. These facies associations precisely revealed that the Crocker Formation's depositional environments were likely deposited in the middle-fan with associated outer-fan settings.
format Article
author Muhd Nur Ismail Abdul Rahman
Hafeez Jeofry
Muhammad Abdullah
Ismail Abd Rahim
Sanudin Hj.Tahir
author_facet Muhd Nur Ismail Abdul Rahman
Hafeez Jeofry
Muhammad Abdullah
Ismail Abd Rahim
Sanudin Hj.Tahir
author_sort Muhd Nur Ismail Abdul Rahman
title Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia
title_short Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia
title_full Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia
title_fullStr Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia
title_full_unstemmed Facies analysis of the Late Eocene deep-marine middle- to outer-fan sequence of the Crocker Formation in Tenom District, Sabah, Malaysia
title_sort facies analysis of the late eocene deep-marine middle- to outer-fan sequence of the crocker formation in tenom district, sabah, malaysia
publisher Persatuan Geologi Malaysia
publishDate 2021
url https://eprints.ums.edu.my/id/eprint/31870/2/Facies%20analysis%20of%20the%20Late%20Eocene%20deep-marine%20middle-%20to%20outer-fan%20sequence%20of%20the%20Crocker%20Formation%20in%20Tenom%20District%2C%20Sabah%2C%20Malaysia_ABSTRACT.pdf
https://eprints.ums.edu.my/id/eprint/31870/1/Facies%20analysis%20of%20the%20Late%20Eocene%20deep-marine%20middle-%20to%20outer-fan%20sequence%20of%20the%20Crocker%20Formation%20in%20Tenom%20District%2C%20Sabah%2C%20Malaysia.pdf
https://eprints.ums.edu.my/id/eprint/31870/
https://gsm.org.my/products/702001-101922-PDF.pdf
http://dx.doi.org/10.7186/bgsm72202105
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