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...
| Asıl Yazarlar: | , , |
|---|---|
| Materyal Türü: | Makale |
| Dil: | English |
| Baskı/Yayın Bilgisi: |
Departmen Teknik Geologi
2015
|
| Konular: | |
| Online Erişim: | https://repository.ugm.ac.id/135514/1/GEO118%20Paper%20Semnas%20UGM%202015%20STT%20Migas.pdf |
| _version_ | 1826049388174114816 |
|---|---|
| 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 |
| collection | UGM |
| 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. |
| first_indexed | 2024-03-13T23:45:11Z |
| format | Article |
| id | oai:generic.eprints.org:135514 |
| institution | Universiti Gadjah Mada |
| language | English |
| last_indexed | 2024-03-13T23:45:11Z |
| publishDate | 2015 |
| publisher | Departmen Teknik Geologi |
| record_format | dspace |
| spelling | oai:generic.eprints.org: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. |
| 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 |
| 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_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_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_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 |
| topic | Geology |
| url | https://repository.ugm.ac.id/135514/1/GEO118%20Paper%20Semnas%20UGM%202015%20STT%20Migas.pdf |
| work_keys_str_mv | AT rizkiputraptratamarizkiputraptratama unlockingheterogeneticreservoirbyusingsequencestratigraphyonsandyfluvialdepositsofthemiddlebalikpapanformationoutcropsamarindakuteibasinitsimplicationforreservoirdistribution AT diponegoroariwibowodiponegoroariwibowo unlockingheterogeneticreservoirbyusingsequencestratigraphyonsandyfluvialdepositsofthemiddlebalikpapanformationoutcropsamarindakuteibasinitsimplicationforreservoirdistribution AT zakariayahyazakariayahya unlockingheterogeneticreservoirbyusingsequencestratigraphyonsandyfluvialdepositsofthemiddlebalikpapanformationoutcropsamarindakuteibasinitsimplicationforreservoirdistribution |