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  • 1
    Online-Ressource
    Online-Ressource
    Canadian Center of Science and Education ; 2019
    In:  Modern Applied Science Vol. 13, No. 8 ( 2019-07-25), p. 22-
    In: Modern Applied Science, Canadian Center of Science and Education, Vol. 13, No. 8 ( 2019-07-25), p. 22-
    Kurzfassung: A detailed stratigraphy description and measurements of the sedimentary facies within the Halang Formation has been carried out to provide a thorough assessment of the architectural facies and depositional environment. The study area is located along the Tajum River in the District of Gumelar, Banyumas, Central Java-Indonesia where most of the Halang Formation is preserved in a good condition. Three cycles of facies association from basin plain, in channel to channel overbank deposits were able to be determined from the formation which indicate very active changes of sub-depositional environment that related to transgressive response influenced by the local tectonic during sedimentation takes place.
    Materialart: Online-Ressource
    ISSN: 1913-1852 , 1913-1844
    Sprache: Unbekannt
    Verlag: Canadian Center of Science and Education
    Publikationsdatum: 2019
    ZDB Id: 2436317-0
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  • 2
    Online-Ressource
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    Insight Society ; 2021
    In:  International Journal on Advanced Science, Engineering and Information Technology Vol. 11, No. 3 ( 2021-06-30), p. 1268-
    In: International Journal on Advanced Science, Engineering and Information Technology, Insight Society, Vol. 11, No. 3 ( 2021-06-30), p. 1268-
    Materialart: Online-Ressource
    ISSN: 2460-6952 , 2088-5334
    Sprache: Unbekannt
    Verlag: Insight Society
    Publikationsdatum: 2021
    ZDB Id: 2687619-X
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  • 3
    Online-Ressource
    Online-Ressource
    Ikatan Ahli Geologi Indonesia ; 2021
    In:  Berita Sedimentologi Vol. 47, No. 3 ( 2021-12-28), p. 43-49
    In: Berita Sedimentologi, Ikatan Ahli Geologi Indonesia, Vol. 47, No. 3 ( 2021-12-28), p. 43-49
    Kurzfassung: In Indonesia, nannofosils are commonly used for age estimation on Miocene marine sediment, but they are rarely performed on Quaternary sediment. This paper introduces two nannofossil biozones, Martini (1971) and Backman et al. (2012) and the comparison between the two biozones. An uninterrupted interval of marine sediments was described and picked for quantitative nannoplankton analysis. The samples were taken from Ledok Formation to Lidah Formation in Pati Region, Northeast Java Basin. The samples were prepared by quick smear slides method and and analyzed by quantitative field of view method. Martini (1971) biozone can be used to subdivide the Late Miocene–Pleistocene sediments into 5 biozones, but Backman et al. (2012) can be used to classify the same sediments into 8 biozones. The biozone subdivision from Backman et al. (2012) is more detailed than that of Martini (1971) because an updated dating and biozone in the three new dating zone data.
    Materialart: Online-Ressource
    ISSN: 0853-9413
    Sprache: Unbekannt
    Verlag: Ikatan Ahli Geologi Indonesia
    Publikationsdatum: 2021
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  • 4
    Online-Ressource
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    National Research and Innovation Agency ; 2018
    In:  RISET Geologi dan Pertambangan Vol. 28, No. 2 ( 2018-11-21), p. 129-
    In: RISET Geologi dan Pertambangan, National Research and Innovation Agency, Vol. 28, No. 2 ( 2018-11-21), p. 129-
    Kurzfassung: The detail taxonomy analysis was performed to classify Acropora corals in Ujunggenteng Area. The research area was selected because the continuously exposed Quaternary coralline limestones, indicated the high variation and wide distribution of coral fossils. Moreover, the facies changes and contacts with shoreface sediments were clearly observed in this area. Detail taxonomy based on morphological description can classify Acropora corals in Ujunggenteng area into four species: Acropora cervicornis, Acropora palifera, Acropora gemmifera, and Acropora humilis. The study of coral paleontology and the application of the presence of corals as a standard facies belt were still rarely performed in Indonesia. Previous studies classified the coralline limestone into one standard facies belt, which was the organic build- up standard facies belt. Another approach was required to capture many conditions of coral fossil occurrences; not only in build-up condition but also in transported condition. Therefore, another purpose of this study is to modify the standard facies belt with a different approach using coral taphonomy and sediment association.Analisis taksonomi secara detil dilakukan untuk mengklasifikasikan koral Acropora di daerah Ujunggenteng. Daerah penelitian dipilih karena tersingkapnya batugamping terumbu berumur Kuarter yang menerus, yang menunjukkan tingginya jumlah spesies dan distribusi fosil koral yang luas. Selain itu, perubahan fasies dan kontak dengan batupasir pantai dapat jelas diamati pada daerah ini. Taksonomi detil berdasarkan deskripsi morfologi dapat mengelompokkan koral Acropora di daerah Ujunggenteng menjadi empat spesies: Acropora cervicornis, Acropora palifera, Acropora gemmifera, dan Acropora humilis. Selain itu, studi mengenai paleontologi dan penggunaan kehadiran koral sebagai dasar pembagian sabuk standar fasies batugamping masih jarang dilakukan di Indonesia. Studi sebelumnya mengelompokkan batugamping terumbu menjadi satu sabuk standar fasies, yaitu organic build up. Pendekatan yang lain diperlukan untuk menjelaskan kondisi koral lainnya pada batugamping, tidak hanya dalam kondisi tumbuh, tetapi juga dalam kondisi tertransportasi. Oleh karena itu, penelitian ini bertujuan untuk memodifikasi sabuk standar fasies dengan pendekatan berbeda menggunakan tafonomi koral dan asosiasi sedimen. 
    Materialart: Online-Ressource
    ISSN: 2354-6638 , 0125-9849
    Sprache: Unbekannt
    Verlag: National Research and Innovation Agency
    Publikationsdatum: 2018
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  • 5
    Online-Ressource
    Online-Ressource
    Insight Society ; 2019
    In:  International Journal on Advanced Science, Engineering and Information Technology Vol. 9, No. 2 ( 2019-04-07), p. 594-
    In: International Journal on Advanced Science, Engineering and Information Technology, Insight Society, Vol. 9, No. 2 ( 2019-04-07), p. 594-
    Materialart: Online-Ressource
    ISSN: 2460-6952 , 2088-5334
    Sprache: Unbekannt
    Verlag: Insight Society
    Publikationsdatum: 2019
    ZDB Id: 2687619-X
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  • 6
    Online-Ressource
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    National Research and Innovation Agency ; 2014
    In:  Jurnal RISET Geologi dan Pertambangan Vol. 24, No. 1 ( 2014-05-20), p. 1-
    In: Jurnal RISET Geologi dan Pertambangan, National Research and Innovation Agency, Vol. 24, No. 1 ( 2014-05-20), p. 1-
    Materialart: Online-Ressource
    ISSN: 2354-6638 , 0125-9849
    Sprache: Unbekannt
    Verlag: National Research and Innovation Agency
    Publikationsdatum: 2014
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  • 7
    Online-Ressource
    Online-Ressource
    National Research and Innovation Agency ; 2017
    In:  RISET Geologi dan Pertambangan Vol. 27, No. 2 ( 2017-12-21)
    In: RISET Geologi dan Pertambangan, National Research and Innovation Agency, Vol. 27, No. 2 ( 2017-12-21)
    Kurzfassung: Biofacies concept was proposed to approach the carbonate facies determination by using coral species description and ecology reconstruction. Ujunggenteng area was selected for this study because it has modern carbonate rocks with continues distribution and contains many well-preserved coral fossils. Ujunggenteng area can be distinguished into three biofacies: Acropora cervicornis – Acropora palifera biofacies, Acropora gemmifera – Acropora humilis biofacies, and Acropora cervicornis – Acropora palmata biofacies. The paleobathymetry analysis had indicated that Acropora cervicornis – Acropora palifera biofacies grew in the deepest environment, between 8 – 13 meters depth. Acropora gemmifera – Acropora humilis biofacies lived in a shallower environment between 3 – 8 meters depth, and Acropora cervicornis – Acropora palmata biofacies was deposited between 0 – 3 meters. The Mg/Ca trend showed a negative correlation with the paleobathymetry result. Decreasing Mg/Ca ratio was related to increasing paleobathymetry. Acropora cervicornis – Acropora palifera biofacies has the smallest Mg/Ca ratio, between 14 – 15 mmol. Acropora gemmifera – Acropora humilis biofacies has Mg/Ca ratio between 17 – 21 mmol.  Acropora cervicornis – Acropora palmata biofacies has the highest Mg/Ca ratio, between 23 – 24 mmol. Mg/Ca ratio value was related to paleotemperature, in which the decreasing of Mg/Ca ratio associated to decreasing paleotemperature.Konsep biofasies dipilih dan diajukan sebagai salah satu pendekatan untuk penentuan fasies karbonat. Daerah Ujunggenteng dipilih untuk studi ini karena daerah ini menunjukkan perkembangan batuan karbonat yang menerus dan fosil koral yang terawetkan dengan baik. Daerah Ujunggenteng dapat dibagi menjadi tiga biofasies, yaitu biofasies Acropora cervicornis – Acropora palifera, biofasies Acropora gemmifera – Acropora humilis biofacies, dan biofasies Acropora cervicornis – Acropora palmata. Analisis paleobatimetri menunjukkan bahwa biofasies Acropora cervicornis – Acropora palifera tumbuh di lingkungan yang paling dalam, yaitu 8 – 13 meter. Biofasies Acropora gemmifera – Acropora humilis hidup di lingkungan yang lebih dangkal, yaitu 3 – 8 meter, dan biofasies Acropora cervicornis – Acropora palmata terendapkan di lingkungan yang lebih dangkal, yaitu 0 – 3 meter. Analisis kadar Mg/Ca menunjukkan nilai yang berlawanan dengan paleobatimetri. Penurunan kadar Mg/Ca memiliki hubungan dengan peningkatan paleobatimetri. Biofasies Acropora cervicornis – Acropora palifera memiliki nilai kadar Mg/Ca paling rendah, yaitu 14 – 15 mmol. Biofasies Acropora gemmifera – Acropora humilis memiliki kadar Mg/Ca yang lebih tinggi dibandingkan dengan biofasies Acropora cervicornis – Acropora palifera, yaitu 17 – 21 mmol. Biofasies Acropora cervicornis – Acropora palmata menunjukkan nilai kadar Mg/Ca yang paling tinggi, yaitu 23 – 24 mmol. Kadar Mg/Ca memiliki hubungan dengan perubahan paleotemperatur. Penurunan kadar Mg/Ca berasosiasi dengan penurunan paleotemperatur.
    Materialart: Online-Ressource
    ISSN: 2354-6638 , 0125-9849
    Sprache: Unbekannt
    Verlag: National Research and Innovation Agency
    Publikationsdatum: 2017
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  • 8
    Online-Ressource
    Online-Ressource
    National Research and Innovation Agency ; 2018
    In:  RISET Geologi dan Pertambangan Vol. 28, No. 2 ( 2018-11-27), p. 251-
    In: RISET Geologi dan Pertambangan, National Research and Innovation Agency, Vol. 28, No. 2 ( 2018-11-27), p. 251-
    Kurzfassung: The upper part of Tapak Formation in Kali Cimande consists of alternating sandstones, siltstone and mudstone. The alternating sequence showed a fining and thinning upward bedding pattern. The facies association of the alternation built up by sand flat facies, which characterized by medium sandstone, moderate sorted, with cross-lamination sedimentary structures and mostly on the top of sandstone layer found a bioturbation trace fossils (Skolithos). Mixed flat facies, which is characterized by an alternation of thin layered sandstones with mudstone and siltstone, with lenticular, wavy, and flaser sedimentary structures, contained many forms of bioturbation, such Planolites, Thallasinoides, Lockeia, and Ophiomorpha. Mud flat facies association, is characterized by a repeated of claystone with thin sandstone intercalation, where the ratio of clay content more than 95 % of the total layers, contained abundantly with trace fossil Lockeia. Upper Tapak Formation plays as moderate reservoir potential. The thick sandstone in sand flat facies with moderate to poorly sorted and moderate porosity is required to provide hydrocarbon flows in Banyumas Basin.Bagian atas Formasi Tapak di Kali Cimande terdiri dari perselingan batupasir-batulanau dan mudstone. Sekuen perselingan menunjukkan pola perlapisan menghalus dan menipis ke atas. Asosiasi fasies tersebut terdiri dari fasies sand flat, yang dicirikan oleh batu pasir sedang, pemilahan sedang, struktur sedimen silang-siur serta fosil jejak bioturbasi (Skolithos) pada bagian puncak kebanyakan lapisan batu pasir. Fasies mixed flat, dicirikan oleh perselingan batupasir berlapis tipis dengan mudstone dan batulanau, serta struktur sedimen lentikular, perlapisan bergelombang, dan flaser, mengandung banyak bioturbasi, seperti Planolites, Thallasinoides, Lockeia, serta Ophiomorpha. Asosiasi Fasies sand flat, dicirikan oleh perulangan batulempung dengan sisipan batupasir tipis, dengan kandungan lempung lebih dari 95% total lapisan, serta fosil jejak Lockeia yang melimpah. Formasi Tapak Atas berperan sebagai reservoir potensial sedang. Bagian batupasir tebal di fasies sand flat dengan pemilahan sedang hingga buruk dan porositas sedang diperlukan untuk menyediakan aliran hidrokarbon di Cekungan Banyumas.  
    Materialart: Online-Ressource
    ISSN: 2354-6638 , 0125-9849
    Sprache: Unbekannt
    Verlag: National Research and Innovation Agency
    Publikationsdatum: 2018
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  • 9
    In: Earthquake Science, Elsevier BV, Vol. 30, No. 2 ( 2017-4), p. 107-113
    Materialart: Online-Ressource
    ISSN: 1674-4519 , 1867-8777
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2017
    ZDB Id: 2245562-0
    ZDB Id: 1340406-4
    ZDB Id: 2488159-4
    SSG: 16,13
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  • 10
    In: IOP Conference Series: Earth and Environmental Science, IOP Publishing, Vol. 71 ( 2017-06), p. 012001-
    Materialart: Online-Ressource
    ISSN: 1755-1307 , 1755-1315
    Sprache: Unbekannt
    Verlag: IOP Publishing
    Publikationsdatum: 2017
    ZDB Id: 2434538-6
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