Proceedings of the International Conference on Tropical Studies and Its Application (ICTROPS 2024)

Sedimentation Dynamics of Senoni Village, Sebulu Sub-District, Kutai Kartanegara District, East Kalimantan Province

Authors
Resty Intan Putri1, Muhammad Amir Masyudi1, *, Koeshadi Sasmito1
1Mulawarman University, Samarinda, East Kalimantan, 75119, Indonesia
*Corresponding author. Email: amirmasyudi2@gmail.com
Corresponding Author
Muhammad Amir Masyudi
Available Online 7 June 2025.
DOI
10.2991/978-94-6463-732-8_8How to use a DOI?
Keywords
Geological Potential; Sedimentation Dynamics; Stratigraphy
Abstract

The research area is in Senoni Village, Sebulu District, Kutai Kartanegara Regency, East Kalimantan Province. It is included in the Kutai Basin in the Pamaluan Formation and Balang Island Formation. Sedimentation dynamics analysis was conducted to illustrate how the stratigraphic conditions in this research area will facilitate further geological studies and plans for the development of the geological potential of the Senoni Village area and its surroundings, especially in the Pamaluan Formation and Balang Island Formation in the Kutai Basin. The method used in this study was carried out by taking lithological data on the surface as outcrops or outcrops in the field with an area of approximately 16 km2. Lithological data taken in the form of lithological description data from several outcrops found in the research area will then be further analyzed in the research area. Based on the research results, seven types of facies form six facies’ associations deposited in the depositional environment of a shelf, Pro-delta, delta front and lower delta plain. Based on the analysis of sedimentation dynamics, namely the stratigraphic sequence, two parasequence sets were gradually deposited. The first is in the Transgressive System Tract (TST) phase with a sediment pattern that smoothes upwards or retrogradation, which above it is bounded by the Maximum Flooding Surface (MFS) interpreted as the formation of crystalline limestone in the study area. The second is the Highstand System Tract (HST) phase, which has a sediment pattern that coarsens upwards or progradates.

Copyright
© 2025 The Author(s)
Open Access
Open Access This chapter is licensed under the terms of the Creative Commons Attribution-NonCommercial 4.0 International License (http://creativecommons.org/licenses/by-nc/4.0/), which permits any noncommercial use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license and indicate if changes were made.

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Volume Title
Proceedings of the International Conference on Tropical Studies and Its Application (ICTROPS 2024)
Series
Advances in Engineering Research
Publication Date
7 June 2025
ISBN
978-94-6463-732-8
ISSN
2352-5401
DOI
10.2991/978-94-6463-732-8_8How to use a DOI?
Copyright
© 2025 The Author(s)
Open Access
Open Access This chapter is licensed under the terms of the Creative Commons Attribution-NonCommercial 4.0 International License (http://creativecommons.org/licenses/by-nc/4.0/), which permits any noncommercial use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license and indicate if changes were made.

Cite this article

TY  - CONF
AU  - Resty Intan Putri
AU  - Muhammad Amir Masyudi
AU  - Koeshadi Sasmito
PY  - 2025
DA  - 2025/06/07
TI  - Sedimentation Dynamics of Senoni Village, Sebulu Sub-District, Kutai Kartanegara District, East Kalimantan Province
BT  - Proceedings of the International Conference on Tropical Studies and Its Application (ICTROPS 2024)
PB  - Atlantis Press
SP  - 70
EP  - 82
SN  - 2352-5401
UR  - https://doi.org/10.2991/978-94-6463-732-8_8
DO  - 10.2991/978-94-6463-732-8_8
ID  - Putri2025
ER  -