UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION

Basically, Sequence stratigraphic concept has used for analyses of seismic cross- sections, well logs and outcrop studies of sedimentary rock are used to predict the thickness, extent of sediment lithology and understanding sediment geometry changes with relative sea level and rates o...

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Main Authors: Rizki Putra Ptratama, Rizki Putra Ptratama, Diponegoro Ariwibowo, Diponegoro Ariwibowo, Zakaria Yahya, Zakaria Yahya
Format: Article PeerReviewed
Language:English
Published: Departmen Teknik Geologi 2015
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Online Access:https://repository.ugm.ac.id/135514/1/GEO118%20Paper%20Semnas%20UGM%202015%20STT%20Migas.pdf
https://repository.ugm.ac.id/135514/
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spelling id-ugm-repo.1355142015-12-30T03:04:23Z https://repository.ugm.ac.id/135514/ UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION Rizki Putra Ptratama, Rizki Putra Ptratama Diponegoro Ariwibowo, Diponegoro Ariwibowo Zakaria Yahya, Zakaria Yahya Geology Basically, Sequence stratigraphic concept has used for analyses of seismic cross- sections, well logs and outcrop studies of sedimentary rock are used to predict the thickness, extent of sediment lithology and understanding sediment geometry changes with relative sea level and rates of sedimentation. The sequence principles can be applied readily to outcrop sources. This paper will fully discuss the sequence stratigraphic concept of heterogenetic facies on Gelingseh formation (Balikpapan Group). The data were collected from the surface outcrops in Simpang pasir area, Samarinda through field geology mapping. Then we continued to a laboratory analysis of said Miocene outcrops within study area. Several individual facies, in terms of deposition events, were determined in the study area. There are 8 facies associations from four stratigraphic logs: 1) Pebbly – Very Coarse Grain Sandstone (Gradding Oriented), 2) Fine Grain Size – Medium Grain Size Massive Sandstone, 3) Massive Mudstone (Shale Clast), 4) Massive Mudstone (Silt Clast), 5) Fine Grain – Coarse Grain through cross bedding Sandstone, 6) Fine Grain – Medium Grain Mud Drapes Associate Cross Lamination Sandstone, 7) Fine Grain – Medium Grain Laminae Sandstone, 8) Coal Seam. According to the integration of all the individual beds, an analysis of the vertical stratum succession, with nearly complete sequences, are observed at the outcrops in the study area. This study has interpreted comprehensive sand deposits in a fluvial deltaic, which will be useful to encourage future exploration and development. Departmen Teknik Geologi 2015-10-29 Article PeerReviewed application/pdf en https://repository.ugm.ac.id/135514/1/GEO118%20Paper%20Semnas%20UGM%202015%20STT%20Migas.pdf Rizki Putra Ptratama, Rizki Putra Ptratama and Diponegoro Ariwibowo, Diponegoro Ariwibowo and Zakaria Yahya, Zakaria Yahya (2015) UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION. PROCEEDING, SEMINAR NASIONAL KEBUMIAN KE-8 Academia-Industry Linkage 15-16 OKTOBER 2015; GRHA SABHA PRAMANA.
institution Universitas Gadjah Mada
building UGM Library
country Indonesia
collection Repository Civitas UGM
language English
topic Geology
spellingShingle Geology
Rizki Putra Ptratama, Rizki Putra Ptratama
Diponegoro Ariwibowo, Diponegoro Ariwibowo
Zakaria Yahya, Zakaria Yahya
UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION
description Basically, Sequence stratigraphic concept has used for analyses of seismic cross- sections, well logs and outcrop studies of sedimentary rock are used to predict the thickness, extent of sediment lithology and understanding sediment geometry changes with relative sea level and rates of sedimentation. The sequence principles can be applied readily to outcrop sources. This paper will fully discuss the sequence stratigraphic concept of heterogenetic facies on Gelingseh formation (Balikpapan Group). The data were collected from the surface outcrops in Simpang pasir area, Samarinda through field geology mapping. Then we continued to a laboratory analysis of said Miocene outcrops within study area. Several individual facies, in terms of deposition events, were determined in the study area. There are 8 facies associations from four stratigraphic logs: 1) Pebbly – Very Coarse Grain Sandstone (Gradding Oriented), 2) Fine Grain Size – Medium Grain Size Massive Sandstone, 3) Massive Mudstone (Shale Clast), 4) Massive Mudstone (Silt Clast), 5) Fine Grain – Coarse Grain through cross bedding Sandstone, 6) Fine Grain – Medium Grain Mud Drapes Associate Cross Lamination Sandstone, 7) Fine Grain – Medium Grain Laminae Sandstone, 8) Coal Seam. According to the integration of all the individual beds, an analysis of the vertical stratum succession, with nearly complete sequences, are observed at the outcrops in the study area. This study has interpreted comprehensive sand deposits in a fluvial deltaic, which will be useful to encourage future exploration and development.
format Article
PeerReviewed
author Rizki Putra Ptratama, Rizki Putra Ptratama
Diponegoro Ariwibowo, Diponegoro Ariwibowo
Zakaria Yahya, Zakaria Yahya
author_facet Rizki Putra Ptratama, Rizki Putra Ptratama
Diponegoro Ariwibowo, Diponegoro Ariwibowo
Zakaria Yahya, Zakaria Yahya
author_sort Rizki Putra Ptratama, Rizki Putra Ptratama
title UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION
title_short UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION
title_full UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION
title_fullStr UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION
title_full_unstemmed UNLOCKING HETEROGENETIC RESERVOIR BY USING SEQUENCE STRATIGRAPHY ON SANDY FLUVIAL DEPOSITS OF THE MIDDLE BALIKPAPAN FORMATION OUTCROP, SAMARINDA, KUTEI BASIN; IT’S IMPLICATION FOR RESERVOIR DISTRIBUTION
title_sort unlocking heterogenetic reservoir by using sequence stratigraphy on sandy fluvial deposits of the middle balikpapan formation outcrop, samarinda, kutei basin; it’s implication for reservoir distribution
publisher Departmen Teknik Geologi
publishDate 2015
url https://repository.ugm.ac.id/135514/1/GEO118%20Paper%20Semnas%20UGM%202015%20STT%20Migas.pdf
https://repository.ugm.ac.id/135514/
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