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All Journal ILMU KELAUTAN: Indonesian Journal of Marine Sciences Jurnal Kelautan Tropis Journal of Tropical Biodiversity and Biotechnology Jurnal Geosains dan Teknologi APPLIED RESEARCH ON CIVIL ENGINEERING AND ENVIRONMENT (ARCEE) Journal of Applied Geology Berita Sedimentologi JURNAL TEKNIK GEOLOGI : Jurnal Ilmu Pengetahuan dan Teknologi Jurnal Jalan Jembatan Scientific Contributions Oil and Gas
Didit Hadi Barianto
Department Of Geological Engineering, Faculty Of Engineering, Universitas Gadjah Mada, Jl. Grafika Bulaksumur No.2, Sleman, Yogyakarta 55284
Agriculture, Biological Sciences & Forestry Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Earth & Planetary Sciences Energy Engineering Environmental Science Immunology & microbiology Materials Science & Nanotechnology Transportation

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Microfacies and paleoenvironmental study of Limestone of the Peneta Formation from Kerinci Area Akmaluddin, Akmaluddin; Nurhidayah, Efrilia Mahdilah; Agustin, Muhammad Virgiawan; Wirakusuma, Fadhil; Novian, Moch. Indra; Barianto, Didit Hadi
Jurnal Kelautan Tropis Vol 27, No 2 (2024): JURNAL KELAUTAN TROPIS
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/jkt.v27i2.22263

Abstract

The research location is the Tebing Tinggi Village, Kerinci region - Jambi, part of the Barisan Zone. This study focuses on the limestone of the Peneta Formation, which is part of the Pre-Tertiary age. The research will investigate the characteristics of carbonate rocks in the Peneta Formation, including the developed facies, fossil content, and the diagenesis process in the Peneta Formation using field data, petrography, and XRD. Our research has succeeded in dividing the Limestone of the Peneta Formation into 3 lithofacies in the study area, including dismicrite, dolomitic limestone, and meta-mudstone. The lack of marine organisms and the dominance of the mudstone facies indicate that the limestone of the Peneta Formation was deposited in an evaporite or brackish zone environment. The limestone diagenesis process was also confirmed in this study. The research location is included in the mesogenesis stage due to the presence of foliation structures, decussate texture, and dolomite minerals until the telogenesis stage, which is characterized by sparite calcite blocky. Furthermore, forsterite and diaspore minerals were also identified through petrographic and XRD analysis, indicating the occurrence of metamorphic processes at our research location.
Bioerosion in the Late Eocene Discocyclina discus sowerbyi (Nuttall, 1926) in Bayat Area, Indonesia: Implications for Paleoecology Rahmawati, Diana; Surjono, Sugeng Sapto; Barianto, Didit Hadi; Rahardjo, Wartono
Journal of Tropical Biodiversity and Biotechnology Vol 9, No 4 (2024): December
Publisher : Universitas Gadjah Mada

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22146/jtbb.93779

Abstract

This paper discusses about the bioerosion discovered in carbonate tests of Discocyclina discus sowerbyi (Nuttall, 1926), a large benthic foraminifera from the Priabonian (Late Eocene). The study material was sampled from the Gamping beds in the Wungkal-Gamping Formation in Bayat, Indonesia. We discovered four bioerosional trace fossils from three different ichnogenera demonstrate bioerosion from the surface test analysis. Oichnus simplex and Oichnus paraboloides are ichnogenus Oichnus diagnostic drilling holes that are often found on the surface. Caulostrepsis isp. exhibits the presence of uncomplicated U-shaped borings. The observed formation of drill holes can be mostly linked to the predatory behaviour of gastropods, while other trace fossils are predominantly associated with the burrowing activities of worms. The occurrence of well-preserved individual tests exhibiting no signs of bioerosion is infrequently observed in D. discus sowerbyi. In addition, bioerosion occurs more frequently in the microspheric generation than in the megalospheric generation. This research also demonstrates for the first time in Indonesia that parrotfish bite marks have developed on individual tests of the microspheric generation of D. discus sowerbyi. The taphonomic characteristics exhibited by the bioeroded and encrusted D. discus sowerbyi specimens can serve as reliable paleoecological indicators for sediment deposition occurring at an intermediate to high sedimentation regime. The occurrence of larger foraminifera with some bioerosional trace fossil highly proficient at documenting shallow marine sclerobionts. 
Planktonic Foraminifera Biostratigraphy of the Pliocene Kintom and Bongka Formation, Central Sulawesi, Indonesia Novian, Moch. Indra; Barianto, Didit Hadi; Husein, Salahuddin; Surjono, Sugeng Sapto
Journal of Tropical Biodiversity and Biotechnology Vol 9, No 4 (2024): December
Publisher : Universitas Gadjah Mada

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22146/jtbb.94685

Abstract

The Pliocene sediments exposed in the eastern arm of southern Sulawesi consist of Kintom and Bongka Formations, thought to be the result of collisions in the Middle Miocene. The research area is located along the Matindok – OndoOndolu road, Banggai Regency, Central Sulawesi Province. The aims of the research is to determine the rock units that developed in the Kintom – Bongka Formation and determine the chronological time frame based on planktonic foraminifera biostratigraphy. This research used stratigraphic measurement on a scale of 1:100 and Plio-Pleistocene planktonic foraminifera biostratigraphy. A lithological column along 315 meters divided into three rock units. The marl unit and calcareous sandstone unit show characteristics similar to flysch deposits from the collision and are part of the Kintom Formation. Intergrade conglomerate gravelly sandstone deposited unconformably on top of the previous unit is part of the Bongka Formation. This last unit shows characteristics similar to molasse deposits. In total of 46 rock samples were analyzed for foraminifera biostratigraphy. Seven foraminifera biozones showing the age of rock deposition from the Early Pliocene to the Late Pleistocene.The order of the foraminifera biozone is Globorotalia tumida Brady LOZ (PL1a; 5.59 - 4.45 Ma), Globoturborotalita nepenthes Todd CRZ (PL1b; 4.45 - 4.39 Ma), Globotalia acostaensis Blow PRZ (PL2a; 4.39 – 4.31 Ma), Globotalia margaritae Bolli HOZ (PL2b; 4.31 - 3.85 Ma), Sphaeroidinellopsis seminulina Schwager HOZ (PL 3-4; 3.85 – 3.20 Ma), Globorotalia (M) miocenica Palmer/Globorotalia miocenica Palmer HOZ (PL5–6; 3.20 – 2.30 Ma), and Pulleniatina praecursor Banner & Blow HOZ (PL6–PT1a; 2.30 – 2.26 Ma).
Potensi Geosite Kawasan Gunung Penanggungan, Kabupaten Mojokerto, Jawa Timur Sebagai Landasan Penentuan Kawasan Geokonservasi Purnomo Putra, Bagaskara Wahyu; Hendratno, Agus; Barianto, Didit Hadi; Dalimunthe, Hasnan Luthfi
Jurnal Geosains dan Teknologi Vol 7, No 2 (2024): Oktober 2024
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/jgt.7.2.2024.143-164

Abstract

Gunung Penanggungan merupakan gunungapi Kuarter di Jawa Timur yang unik karena memiliki geosite berkaitan dengan situs cagar budaya. Namun, eksistensi Kawasan Gunung Penanggungan berada di ambang kerusakan karena kegiatan ekstraksi bahan galian C dan pembangunan kawasan pabrik di sekitarnya. Untuk melindungi Kawasan Gunung Penanggungan, perlu dilakukan identifikasi potensi geosite sebagai landasan penentuan kawasan geokonservasi. Identifikasi potensi geosite menggunakan Standar Nasional inventarisasi dan identifikasi geosite dari Pusat Survei Geologi, Badan Geologi dan perhitungan kelayakan geosite dengan metode analytical hierarchy process (AHP) serta mempertimbangkan hasil survei lapangan. Berdasarkan hasil penelitian, Kawasan Gunung Penanggungan terbagi menjadi lima satuan geomorfologi yang tersusun atas tujuh satuan litologi. Hasil inventarisasi dan identifikasi geosite menghasilkan 29 geosite diantaranya geosite Candi Kendalisodo, geosite Petirtaan Jolotundo, dan geosite Candi Wayang yang memiliki nilai saintifik, nilai konservasi dan nilai kebudayaan menonjol, sehingga geosite pada Kawasan Gunung Penanggungan termasuk dalam stone heritage. Hasil perhitungan AHP potensi geosite Kawasan Gunung Penanggungan menunjukkan tingkat potensi sedang hingga tinggi untuk mendukung Kawasan Gunung Penanggungan sebagai kawasan geokonservasi.
LATE CRETACEOFS SEDIMENTARY ROCK IN BARITO BASIN, INDONESIA: LITHOLOGY, PALEONTOLOGY, AND PALEOENVIRONMENT Akmaluddin Akmaluddin; Muhammad Virgiana A; Salahuddin Husein; Muhammad I. Novian; Nugroho I. Setiawan; Didit Hadi Barianto; Sunjaya E.S.; Banti T. Tampubolon
Scientific Contributions Oil and Gas Vol 42 No 3 (2019)
Publisher : Testing Center for Oil and Gas LEMIGAS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29017/SCOG.42.3.400

Abstract

The Barito Basin so far known as back-arc basin that formed by the rifting in Early Tertiary, which the oldest sedimentary rock in this basin is believed has a Middle Eocene to Early Oligocene age. However, this research will present new evidence regarding the existence of sedimentary rocks that are older than Cenozoic age in the Barito Basin. This research was carried out on Bongkang-2 well, as the main data, and other five wells which have an indication of the discovery of Pre-Tertiary sedimentary rocks, which are generally located in the northern part of the Barito Basin. Integration of mud log data, petrography, paleontology, and dip-meter data, resulting the identification of lithology, age and depositional environment, and then interpretation of the paleoenvironment of the Barito Basin in the Late Cretaceous is carried out. Based on the analysis of data, it is show that Pre-Tertiary sedimentary rocks found in the six wells analyzed has Cenomanian age, which is indicated by the presence of large foraminifera fossils in the form of Sulcoperculina sp. and Orbitolina sp. in Bongkang-2, Hayup-1 and Hayup-3 wells, as well as palynomorph fossils in the form of Cicatrico- sisporites dorogensis, A. tricornitatus, Aquilapollenites sp., Distaverrusporites margaritus and Classopolis cf. classoides in Bagok-1 and Bagok-2 wells. In addition, based on lithological analysis, in the Bongkang-2, Hayup-1 and Hayup-2 wells lithology develops in the form of limestone, shale and sandstone, while in the Didi-1, Bagok-1 and Bagok-2 wells lithology develops in the form of shale with sandstone and pyroclastic – volcaniclastics rock intercalation. Then, based on the integration of lithology and paleontology analysis, it is known that in the Cenomanian age, terrestrial environments developed in the western part of the Barito Basin, while in the eastern part the shallow marine environment developed.
Co-Authors Adesti Audina Ulfah Agus Hendratno Agustin, Muhammad Virgiawan Akmaluddin Akmaluddin Akmaluddin Akmaluddin Akmaluddin Akmaluddin Akmaluddin Akmaluddin Ali, Che Aziz Banti T. Tampubolon Banti T.Tampubolon Citayana Fani Refalta Dalimunthe, Hasnan Luthfi Dian Novita Diana Rahmawati Diana Rahmawati Donan Satria Yudha Donan Satria Yudha Dwikorita Karnawati E.S., Sunjaya Husein, Salahuddin I Gde Budi Indrawan Inderawan, Gde Budi Koichiro Watanabe Koichiro Watanabe, Koichiro Kuncoro, Pentatok Mochammad Indra Novian Muhammad Ageng Prabowo Muhammad I. Novian Muhammad I.Novian Muhammad Virgiana A Muhammad Virgiana A Novian, Muhammad I. Nugroho I. Setiawan Nugroho I. Setiawan Nurhidayah, Efrilia Mahdilah Pentatok Kuncoro Putra, Bagaskara Wahyu Purnomo Rahardjo, Wartono Rahmadi Hidayat Rusyad Adi Suriyanto Salahuddin Husein Salahuddin Husein Saripudin, Asep Setiawan, Nugroho I. Sudarno, Ignatius Sugeng Sapto Surjono Sunjaya E.S. Sunjaya E.S. Tampubolon, Banti T. Tri Puji Astuti Tri Puji Astuti Virgiana A, Muhammad Wahyu Wilopo Wartono Rahardjo Wirakusuma, Fadhil