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Contact Name
Aldis Ladesta
Contact Email
aldis@trisakti.ac.id
Phone
+6285711947547
Journal Mail Official
aldis@trisakti.ac.id
Editorial Address
Fakultas Teknologi Kebumian dan Energi Universitas Trisakti, Jakarta Gedung D Lt. 2, Kampus A Jl. Kyai Tapa Grogol Jakarta 11440, Indonesia Telephone: +62-21-5663232 ext 8520
Location
Kota adm. jakarta barat,
Dki jakarta
INDONESIA
Journal of Geoscience Engineering and Energy (JOGEE)
Published by Universitas Trisakti
ISSN : 27155358     EISSN : 27226530     DOI : https://doi.org/10.25105/jogee.v3i2.13860
The main aim of the Journal Geoscience Engineering and Energy (JOGEE) is to provide an open access platform to the articles that resulted of high-quality research works related with the geoscience and energy field. This is open for papers of geology (petrology; volcanology and geothermal; sedimentology and stratigraphy; paleontology; structural geology and seismology; petroleum geosciences; mineral deposits and coal mining; remotee sensing,; hidrogeology; marine geology and oceanography; geological engineering; environmental and geohazard mitigation; and also geotourism), geophysics (physical geology; exploration Geophysics), geochemistry, energy of renewable (geothermal; ..)and non-renewable energy (petroleum engineering; G&G method; mineral deposits, coal and energy resources management),dll. The Journal Geoscience Engineering and Energy (JOGEE) welcome the submission of manuscripts that meet the general criteria of significance and scientific excellence. It caters to the requirements of the geologist, researchers, academicians and also students, lab professional, and industry that is involved in geoscience studies. This journal publishes 2 numbers per year at least 8-9 articles. Papers will be published approximately 14 days after acceptance.
Articles 139 Documents
ANALISIS STABILITAS LERENG UNTUK PERENCANAAN BENDUNGAN JLANTAH DI DESA TLOBO, KECAMATAN JATIYOSO, KABUPATEN KARANGANYAR PROVINSI JAWA TENGAH: SLOPE STABILITY ANALYSIS IN THE JLANTAH DAM PLANNING AT TLOBO VILLAGE, JATIYOSO SUB – DISTRICT, KARANGANYAR DISTRICT, CENTRAL JAVA PROVINCE Dwi Saputra, Zanuar; Ronoatmojo, Imam Setaiji
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.16060

Abstract

Stabilitas lereng merupakan faktor utama yang harus diperhatikan dalam kegiatan perencanaan pembangunan PT. Virama Karya yang terletak pada kecamata Jatiyoso, di karenakan dapat mengganggu kelancaran pembangunan dan dapat membahayakan keselamatan pekerja hal – hal yang dapat menyebabkan leren tidak stabil antara lain yaitu gempa bumi, struktur geologi, peledakan, dan material batuan penyusun lereng, pada penelitian ini dapat menggunakan metode RMR, SMR, dan GSI untuk dapat mengindentifikasikan dan memberikan rekomendasi terhadap kondisi lereng, kemudian menggunakan metode Janbu untuk mendapatkan hasil dari nilai faktor keamanan, pada penelitian ini didapatkan hasil pengukuran geometri lereng yang didapatkan dengan nilai Single Slope 50, tinggi 50 meter, lebar 80 meter, panjang jenjang Slope stability is an important factor that is considered on the bridge which is one of the accesses in the construction of hydropower at the JatiGede dam because it can interfere with the smooth transportation of materials in the construction of hydropower, things that can cause slopes to become unstable are earthquakes, geological structures, and materials. In this study, the slope compilers used the RMR and GSI methods to identify and provide recommendations for slope conditions, then used the Janbu method to obtain the safety factor value, in this study the rock mass conditions on scanlines 1 to 5 were very blocky and rough surface conditions. , weathered rock condition, the safety factor value on the slope is 0.497, and has a sliding wedge type landslide potential of 21.54%. Based on the recommendation slopes made with Slide 6.0 software in order to get a FK value> 1.25 to produce stable slope conditions and can minimize the dangers that can occur.
ANALISIS GEOKIMIA AIR DARI MANIFESTASI PERMUKAAN PADA PROSPEK PANASBUMI FF, KABUPATEN CIANJUR, PROVINSI JAWA BARAT: GEOCHEMISTRY WATER ANALYSIS FROM SURFACE MANIFESTATIONS AT FF GEOTHERMAL PROSPECT, CIANJUR REGENCY, WEST JAVA PROVINCE Fazli, Faiz; Hendrasto, Fajar; Wijaya, Budi
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.16068

Abstract

Lokasi penelitian prospek panasbumi FF yang terletak di Kabupaten Cianjur, Provinsi Jawa Barat mempunyai sumber daya panas bumi yang berpotensi cukup baik. Penelitian ini dilakukan dengan menggunakan data (sekunder) dari Ditjen Energi Baru Terbarukan dan Konservasi Energi (EBTKE) berupa data geokimia fluida serta isotop stabil untuk menghasilkan suatu model konseptual aliran fluida pada lapangan penelitian. Penelitian ini dilakukan untuk menunjukkan lebih detail melalui data permukaan sehingga dapat memberikan gambaran model untuk panasbumi yang terdapat di daerah FF. Terdapat dua tipe air pada daerah penelitian yaitu peripheral water pada lokasi manifestasi MG01, MG02, dan MG05 serta tipe suphate water pada lokasi manifestasi MG03, dan MG04. Pada lokasi MG01 yang terletak di bagian timurlaut daerah penelitian merupakan zona outflow, sedangkan pada lokasi sekitar puncak gunung (bagian baratdaya daerah penelitian) merupakan zona upflow. Sumber air pada daerah penelitian merupakan sea water berupa tipe immature water. The location of the observation field includes the FF geothermal prospect area, Cianjur Regency, West Java Province which has the potential of geothermal resources. This research was conducted by using secondary data from General Directorate of New Renewable Energy and Energy Conservation (EBTKE) in the form of geochemical and stable isotope data so as to produce a fluid flow conceptual model in the research field. Therefore, this study was conducted to look in more detail through surface data so that it can provide an overview for the geothermal model in the FF area. There are two types of water in the research area, namely peripheral water at the of manifestation location of MG01, MG02, and MG05 and the type of suphate water at the manifestation location of MG03, and MG04. At location MG01 which is located in the northeastern part of the research area is an outflow zone, while the location around the top of the mountain (southwestern part of the study area) is an upflow zone. The water source in the research area is sea water in the form of immature water
ANALISIS SEKUEN STRATIGRAFI BERDASARKAN DATA LOG LAPANGAN “DRK” CEKUNGAN JAWA TIMUR UTARA : ANALYSIS OF SEQUENCE STRATIGRAPHY BASED ON LOG DATA “DRK” FIELD NORTH EAST JAVA BASIN Karima, Dani Rizki; Guntoro, Agus
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.16084

Abstract

Daerah penelitian terletak di Lapangan “DRK” yang berada pada Zona Rembang, Cekungan Jawa Timur Utara. Penelitian ini dilakukan untuk menganalisis kondisi bawah permukaan melalui korelasi sumur dan analisis perkembangan distribusi sedimentasi pada Cekungan Jawa Timur Utara. Penelitian ini menggunakan lima data sumur. Analisis Sikuen Stratigrafi didasarkan dari data log, dimana hasil dari analisis Sikuen Stratigrafi ini dapat diinterpretasikannya Fasies dan Lingkungan Pengendapan pada daerah penelitian. The research area is located in the "DRK" field in the Rembang Zone, North East Java Basin. This study was conducted to analyze the subsurface conditions through well correlation and analysis of the development of sedimentation distribution in the North East Java Basin. This study uses five data wells. Sequence Stratigraphy analysis is based on log data, where the results of this Stratigraphic Sequence analysis can be interpreted by Facies and Depositional Environment in the study area.
ANALISIS STRUKTUR GEOLOGI BERDASARKAN DATA PERMUKAAN DAERAH BANJARHARJO, KABUPATEN BREBES, PROVINSI JAWA TENGAH: GEOLOGICAL STRUCTURE ANALYSIS BASED ON SURFACE DATA OF THE BANJARHARJO REGION, BREBES DISTRICT, CENTRAL JAVA PROVINCE Maulana, Ilham; Triany, Novi
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.16238

Abstract

The research area is administratively located in Banjarharjo Village, Banjarharjo District, Brebes Regency, Central Java Province. Geographically, the research area is located at coordinates 108o 49 '15.4 "- 108o 52' 30.8" East Longitude and 06o 59 "21.8" - 07o 02 '04.8 "LS. The research area is included in The North Central Java Basin (The North Serayu Through/Basin) which is a Back Arc Basin. Based on the stratigraphic and sedimentological composition, the research area is classified into five geological units, (old to young), namely: (1) Sandstone and Claystone Interchange Unit, (2) Carbonate Claystone Unit, (3) Sand Limestone Unit, (4) Volcanic Breccia Unit and (5) Andesite Intrusion Unit. According to Pulonggono and Martodjojo (1994) Java Island, there are three straight lines of dominant structure, including: (1) East Laur - Southwest (Meratus Pattern), (2) North - South (Sundanese Pattern) and (3) West - East (Pattern Java). Based on the strike dip and stockiness data at the research location, the results of the force with the direction of the main stress are relatively Northeast-Southwestern, with the combination of Harding modeling, (1977) and Moody and Hill, (1956). The structural arrangements in the research area that are formed are (1) Cibuluh thrust fault, (2) Maibah sinistral strike-slip fault, (3) Cikuya sinistral strike-slip fault, and (4) Cikuya dextral strikeslip fault.
KARAKTERISTIK BATUGAMPING FORMASI WONOSARI DI DAERAH BUNDER DAN SEKITARNYA, WONOSARI,GUNUNGKIDUL D.I.Y : THE CHARACTERISTICS OF THE WONOSARI FORMATION LIMESTONE IN THE BUNDER AREA AND ITS SURROUNDINGS, WONOSARI, GUNUNGKIDUL, D.I.Y Hafiz, Surya Darma; Moehammad Ali Jambak; Budi Wijaya; Mira Meirawaty; Cahyaningratri Prima Ryandhani; Wildan Tri Koesmawardani; Nuryana, Suherman Dwi; Zefanya, Oliver Enrico
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.17301

Abstract

Studi ini bertujuan untuk mengkaji karakteristik  batugamping Formasi Wonosari di Desa Bunder, Kecamatan Ponjong, Kabupaten Gunungkidul, DIY. Analisis litologi mengungkapkan bahwa batuan wackstone berwarna coklat dengan tekstur bioklastik, terdiri dari sekitar 75% lumpur karbonat/mikrit dan 25% fragmen butiran. Kehadiran fosil meliputi foraminifera planktonik dan bentos, dengan fragmen bioklas yang utuh mengalami proses mikritisasi dan neomorfisme menjadi kalsit spar yang jernih. Pengamatan lapangan menunjukkan adanya singkapan batuan yang segar maupun lapuk, dengan jurus lapisan berkisar antara N100° E hingga 105° E dan kemiringan rata-rata sekitar 4° - 8°. Ketebalan perkiraan formasi ini adalah sekitar 150-200 m. Berdasarkan analisis mikropaleontologi, spesies foraminifera planktonik dominan seperti Orbulina universa dan Sphaerodinella subdehiscens mengindikasikan rentang umur antara N10-N18. Satuan ini menunjukkan adanya struktur sedimen berlapis baik dan struktur masif gelegar, menandakan pengendapan di lingkungan yang tenang dengan energi rendah. Penelitian ini memberikan pemahaman lebih baik tentang litologi, lingkungan pengendapan, dan perkiraan umur Formasi Wonosari di wilayah penelitian. This study focuses on the characteristic of the Wonosari Formation carbonate rocks in Bunder Village, Ponjong Sub-district, Gunungkidul Regency, DIY. The lithological analysis reveals brown-colored wackstone with a bioclastic texture, consisting of 75% mud-supported carbonate/micrite and 25% grain fragments. The fossil assemblage includes planktonic and benthic foraminifera, with intact bioclastic fragments exhibiting signs of micritization and subsequent neomorphism into clear calcite spar. Field observations indicate fresh and weathered outcrops with a bedding strike ranging from N100° E to 105° E and an average dip angle of 4° - 8°. The estimated thickness of the formation is around 150-200 m. Based on micropaleontological analysis, dominant planktonic foraminifera species such as Orbulina universa and Sphaerodinella subdehiscens suggest an age range of N10-N18. The unit displays well-layered sedimentary structures and occasional massive structures, indicating deposition in a low-energy, relatively calm environment. This research contributes to a better understanding of the lithology, depositional environment, and age estimation of the Wonosari Formation in the study area..
ANALISIS JENIS TANAH UNTUK PENENTUAN KAWASAN RESAPAN AIR KELURAHAN KAPUK, KECAMATAN CENGKARENG JAKARTA BARAT: ANALYSIS OF SOIL TYPE FOR DETERMINATION KAPUK DISTRICT WATER ABSOLUTE AREA, CENGKARENG DISTRICT, WEST JAKARTA Ahmad, Riduan; Anugrahadi, Afiat; Yuda, Himmes Fitra
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.17902

Abstract

Water catchment areas in residential areas or in the process of development are very important. The need for water resources that are used to meet the basic needs of personal life as well as development needs that are still growing really need water in the process of infrastructure development Soil type is one of the factors that determines water catchment areas. Soil samples were taken in the study area and then tested in the laboratory to determine the physical properties and classify the types of soil present. The results of the research are that the type of soil in the study area based on USCS is of poor gradation and the type of soil is based on PU No. 02/2013 has a score of 5.
ANALISIS KUALITAS AIR TANAH SUMUR GALI DI DESA KARANGTENGAH, KABUPATEN BOGOR, PROVINSI JAWA BARAT: DUG WELL GROUNDWATER ANALYSIS IN KARANGTENGAH VILLAGE, BOGOR DISTRICT, WEST JAVA PROVINCE Arum, Dannum Sekar; Asseggaf, Abdurrachman; Lestari, Arini Dian
Journal of Geoscience Engineering and Energy VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.18079

Abstract

Air merupakan salah satu kebutuhan pokok manusia yang krusial keberadaannya dalam kehidupan. Pada makalah ini akan dibahas secara lebih terperinci kualitas air tanah yang didapatkan dari pembuatan sumur gali pada Desa Karangtengah, Kabupaten Bogor, Provinsi Jawa Barat. Pada penelitian ini melibatkan pengambilan sampel air pada dua buah sumur gali yang nantinya akan dianalisa lebih lanjut di laboratorium sesuai dengan ketentuan Permenkes No.32 Tahun 2017 mengenai standar baku air bersih, juga mengetahui asal dari air tanah tersebut. Metode yang digunakan dalam penelitian ini adalah eksperimen laboratorium dan analisis hidrogeologi mengenai akuifer yang menyimpan air tanah. Hasil uji laboratorium menunjukan bahwa kedua sumur tersebut tidak memenuhi standar baku mutu air bersih. Air sumur gali 1 memiliki pH sebesar 6,02 sedangkan air sumur gali 2 memiliki kandungan MBAS (Methylene Blue Active Surfactant) sebesar 0,134 yang melebihi batas baku mutu. Air tanah berasal dari akuifer tertekan yang terdiri atas satuan batulempung dan sisipan batupasir. Water is one of the basic human needs that is crucial for its existence in life. This paper will discuss in more detail the quality of groundwater obtained from the construction of dug wells in Karangtengah Village, Bogor Regency, West Java Province. This research involves taking water samples from two dug wells which will be further analyzed in the laboratory in accordance with the provisions of the Minister of Health Regulation No. 32 of 2017 concerning the standard of clean water, as well as knowing the origin of the groundwater. The methods used in this research are laboratory experiments and hydrogeological analysis of aquifers that store groundwater. The results of laboratory tests showed that the two wells did not meet the clean water quality standards. Dug well water 1 has a pH of 6.02 while dug well water 2 has an MBAS (Methylene Blue Active Surfactant) content of 0.134 which exceeds the quality standard limit. Groundwater comes from a confined aquifer consisting of claystone units and sandstone inserts.
ANALISIS BIBLIOMETRIK PERKEMBANGAN MUTAKHIR DALAM STUDI ANISOTROPI SEISMIK (2017 -2022): BIBLIOMETRIC ANALYSIS OF RECENT DEVELOPMENT IN THE SEISMIC ANISOTROPY STUDIES (2017 -2022) Yuda, Himmes Fitra; Ronoatmojo, Imam Setaiji; Burhannudinnur, Muhammad; Nuryana, Suherman Dwi
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.18206

Abstract

The development of seismic anisotropy needs to be studied systematically hence research could be focused on the latest scientific knowledge, therefore a bibliometric analysis is needed as a measurement of citation strength in the form of mapping "co-occurrence", "co-author" and "co- citation", thus the strength of the research direction could be well understood. The software which is used; VOSviewer version 1.6.18 examined at least 494 papers in the SCOPUS domain during 2017 -2020. It appears from the results that the development of the seismic anisotropy are very rapidly dominated by the needs of the applied science and pure science. The heavily publication countries are United States of America, China and Japan. However, in reality, this density does not necessarily correspond to the number of citations between countries, as well with publications in Japan.
DETEKSI ZONA MINERALISASI EMAS DI GUNUNG GUPIT, MAGELANG MENGGUNAKAN METODE INDUCED POLARIZATION: DETECTION OF GOLD MINERALIZATION ZONES IN GUNUNG GUPIT, MAGELANG USING INDUCED POLARIZATION METHOD Yatini; Zakaria, Muhammad Faizal; Putri, Rizkia; Zakaria, Suharwanto
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.18341

Abstract

Mount Gupit is an area with gold mineralization potential which is part of the Menoreh Mountains, in the Magelang area. Mineralization potential mapping was carried out using geophysics, namely the Induced Polarization method. Induced Polarization Method measurements were carried out in 5 trajectories in a relatively west to east direction and with varying path lengths. The configuration used is a dipole-dipole configuration with a: 10 meters and n: 1-6. Interpretation is carried out on the results of the Resistivity and Chargeability data inversion. The inversion results show a resistivity range from 2 to 400 Ohm-m. Resistivity values are divided into three criteria, namely low with a value of less than 10 Ohm-m as clay rock, medium with a range of (10-75) Ohm-m as pyroclastic breccia and high with a value greater than 75 Ohm-m as intrusion or chunks of andesite. The inversion results show that the chargeability value varies from 2 to 80 ms. This value is divided into three criteria, namely low (<10 ms), medium (10 to 35) ms and high (>35 ms). Low chargeability values are interpreted as zones that are not mineralized so that there are no metal minerals. The mineralized zone is being interpreted from a moderate chargeability value. Meanwhile, a high chargeability value is interpreted as a zone that is strongly mineralized and contains significant metallic minerals. The existence of a mineralized zone stretches from track 2 to track 5 to the north, while the zone has disappeared or been exhausted in track 1 to the south of the research area.
IDENTIFIKASI BAHAYA DAN PENILAIAN RISIKO DI KAWASAN WISATA LEUWI KENIT, CILETUH PALABUHANRATU UGG: HAZARD IDENTIFICATION AND RISK ASSESSMENT IN THE LEUWI KENIT TOURISM AREA, CILETUH PELABUHANRATU UGG Surahman, Dikky; Pratiwi, Santi Dwi
Journal of Geoscience Engineering and Energy VOLUME 5, NOMOR 1, FEBRUARI 2024
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v5i1.18669

Abstract

Ciletuh Palabuhanratu as the first geopark in West Java which has been recognized by UNESCO since 2018, is famous as the first land in western Java. One of the natural tourist object in the Geopark area with the beauty of ancient rock structures aged more than 60 million years ago is the Leuwi Kenit natural tourist destination in Pasirpanjang Village, which has a very large number of tourists, but in certain periods there are often visitor accidents. This research aims to identify hazards and risk assessment, as well as risk control from hazards, with research objects including parking areas, entrance gates, access routes, play facilities, and exit routes. The research method is a qualitative Hazard Identification and Risk Assessment and mapping of danger points, literature studies, field observations, interviews with the community, tour guides and tourist attraction guards. Based on the results of the study, there are fifteen danger points in the Leuwi Kenit tourist attraction, some of which can occur when the activity is running with a range of risk relative status, namely low to high. Risk relative high status is recorded to have dominated with seven danger points, risk relative moderate status with six danger points, and risk relative low with two danger points. According to the results of the study, there are fifteen danger points in the Leuwi Kenit tourist attraction, some of which can occur when the activity is running with a range of risk relative status, namely low to high. Risk relative high status is recorded as dominant with seven danger points, risk relative moderate status with six danger points, and risk relative low status with two danger points. The results of the risk assessment show that the risk status is included in potential hazards with high and medium hazard risk levels, management attention and control planning are needed. Alternative risk controls that can be implemented to minimize the occurrence of risk are administrative, engineering, and elimination approaches. Forms of risk avoidance applications such as making paths according to safe standards, making information boards for hazard location points, and rearranging amusement ride according to safety standards at Leuwi Kenit.

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