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All Journal Media Kesehatan Masyarakat Indonesia IJOG : Indonesian Journal on Geoscience SCHOOL EDUCATION JOURNAL PGSD FIP UNIMED Journal of Degraded and Mining Lands Management PENELITIAN DAN KARYA ILMIAH Jurnal Teknologi Mineral dan Batubara Journal of Geoscience, Engineering, Environment, and Technology Abdimas Galuh: Jurnal Pengabdian Kepada Masyarakat JURNAL PENELITIAN DAN KARYA ILMIAH LEMBAGA PENELITIAN UNIVERSITAS TRISAKTI Jurnal Penelitian dan Karya Ilmiah Lembaga Penelitian Universitas Trisakti INDONESIAN JOURNAL OF URBAN AND ENVIRONMENTAL TECHNOLOGY Jurnal AKAL: Abdimas dan Kearifan Lokal Journal of Geoscience Engineering and Energy (JOGEE) JURNAL ABDI MASYARAKAT INDONESIA (JAMIN) Journal of Earth Energy Science, Engineering, and Technology Jurnal Eksakta Kebumian Aceh International Journal of Science and Technology Jurnal Teknologi Mineral dan Batubara Scientific Contributions Oil and Gas
Muhammad Burhannudinnur
Departemen Teknik Geologi Universitas Trisakti
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ANALISIS GEOKIMIA HIDROKARBON SUMUR “FLP” CEKUNGAN JAWA TIMUR UTARA: GEOCHEMICAL ANALYSIS OF HYDROCARBON WELL "FLP" BASIN NORTH EAST JAVA Filipus Armando Armando Ginting; Yarra Sutadiwiria; Cahyaningratri Prima Riyandhani; Muhammad Burhannudinnur; Imam Setiaji Ronoatmojo; Novi Triany
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 4, NOMOR 1, FEBRUARI 2023
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i1.14415

Abstract

Daerah riset terdapat pada Blok Madura, Cekungan Jawa Timur Utara berupa dua sumur FLP-1 dan FLP-2. Analisa dilakukan agar mengetahui karakteristik batuan induk, material organic, biomarker, dan potensi batauan induk(source rock). FLP-1 diketahui terdapat Formasi Tuban dan Formasi Tawun, pada sumur FLP-2 diketahui Formasi Kujung dan Formasi Tuban.indikasi batuan induk potesial (tipe kerogen II) potensi mengenerasikan hidrokarbon jenis utama berupa gas, asal material tumbuhan tingkat tinggi dan lingkungan pengendapan organik fluvio-deltaic. Sumur FLP-2 Formasi Kujung Indikasi batuan induk efektif. (tipe kerogen II/III) potensi menggenerasikan hidrokarbon jenis minyak dan gas, asal material alga dan tumbuhan tingkat tinggi dan fasies organik marine-deltaic.
ANALISIS LINGKUNGAN PENGENDAPAN PADA LAPANGAN AR & RB FORMASI TALANG AKAR, CEKUNGAN SUMATRA SELATAN: ANALYSIS OF DEPOSIT ENVIRONMENT IN AR & RB FIELDS OF THE TALANG AKAR FORMATION, SOUTH SUMATRA BASIN Andreas Rendy Bramantyo; Muhammad Burhannudinnur; wildan Tri K
Jurnal Eksakta Kebumian Vol. 3 No. 1 (2022): JURNAL EKSAKTA KEBUMIAN (JEK)
Publisher : Fakultas Teknologi Kebumian dan Energi, Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jek.v3i1.16444

Abstract

Abstrak Penelitian ini dilakukan pada lapangan AR & RB, formasi Talang Akar, Cekungan Sumatra Selatan. Dimana formasi Talang Akar ini memiliki potensi yang sangat besar dalam memiliki kandungan minyak bumi dan gas di Cekungan Sumatra Selatan ini, namun tidak semudah itu untuk menemukan minyak dan gas, perlu dilakukan analisis yang mendalam dalam melakukan eksplorasi. Salah satu analisis yaitu analisis lingkungan pengendapan. Dalam melakukan analisis ini menggunakan software petrel 2017. Berdasarkan hasil dari pengolahan data menghasilkan bahwa lapangan AR & RB terbentuk pada lingkungan pengendapan fluvial, delta plain dan delta front. Pembagian sekuen pada lapangan ARB terbagi menjadi 3 dan memiliki fasies yaitu flooding surface 1 terdapat fasies fluvial channel, point bar, creavase splay dan floodplain, flooding surface 2 terdapat fasies distributary channel, mouth bar dan mud flat dan flooding surface 3 terdapat fasies mouth bar dan mud flat.   Kata kunci : Lingkungan Pengendapan, Cekungan Sumatra Selatan dan Formasi Talang Akar   Abstract This research was conducted in field AR & RB, Talang Akar formation, South Sumatra Basin. Where the Talang Akar formation has enormous potential in containing oil and gas in the South Sumatra Basin, but did not find it to find oil and gas, in-depth analysis is needed to carry out exploration. One of the analyzes is the analysis of the depotitional environment. In conducting this analysis using petrel 2017 software. Based on the results of data processing, it was found that the AR & RB field was formed in a fluvial, delta plain and delta front environment. Sequence distribution in field ARB is divided into 3 and has facies, namely flooding surface 1 which has fluvial channel, point bar, creavase splay and floodplain facies, flooding surface 2 has distributed channel facies, mouth bar and mud flat and flooding surface 3 has mouth bar and mud flat facies.  Keywords: Depotitional Environment, South Sumatra Basin and Talang Akar Formation
ANALISIS LINGKUNGAN PENGENDAPAN PADA LAPANGAN AR & RB FORMASI TALANG AKAR, CEKUNGAN SUMATRA SELATAN : DUG WELL GROUNDWATER ANALYSIS IN KARANGTENGAH VILLAGE, BOGOR DISTRICT, WEST JAVA PROVINCE Andreas Rendy Bramantyo; Muhammad Burhannudinnur; Wildan Tri Koesmawardani
Journal of Geoscience Engineering & Energy (JOGEE) VOLUME 4, NOMOR 2, AGUSTUS 2023
Publisher : Universitas trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v4i2.16008

Abstract

Penelitian ini dilakukan pada lapangan AR & RB, formasi Talang Akar, Cekungan Sumatra Selatan. Dimana formasi Talang Akar ini memiliki potensi yang sangat besar dalam memiliki kandungan minyak bumi dan gas di Cekungan Sumatra Selatan ini, namun tidak semudah itu untuk menemukan minyak dan gas, perlu dilakukan analisis yang mendalam dalam melakukan eksplorasi. Salah satu analisis yaitu analisis lingkungan pengendapan. Dalam melakukan analisis ini menggunakan software petrel 2017. Berdasarkan hasil dari pengolahan data menghasilkan bahwa lapangan AR & RB terbentuk pada lingkungan pengendapan fluvial, delta plain dan delta front. Pembagian sekuen pada lapangan ARB terbagi menjadi 3 dan memiliki fasies yaitu flooding surface 1 terdapat fasies fluvial channel, point bar, creavase splay dan floodplain, flooding surface 2 terdapat fasies distributary channel, mouth bar dan mud flat dan flooding surface 3 terdapat fasies mouth bar dan mud flat. This research was conducted in field AR & RB, Talang Akar formation, South Sumatra Basin. Where the Talang Akar formation has enormous potential in containing oil and gas in the South Sumatra Basin, but did not find it to find oil and gas, in-depth analysis is needed to carry out exploration. One of the analyzes is the analysis of the depotitional environment. In conducting this analysis using petrel 2017 software. Based on the results of data processing, it was found that the AR & RB field was formed in a fluvial, delta plain and delta front environment. Sequence distribution in field ARB is divided into 3 and has facies, namely flooding surface 1 which has fluvial channel, point bar, creavase splay and floodplain facies, flooding surface 2 has distributed channel facies, mouth bar and mud flat and flooding surface 3 has mouth bar and mud flat facies.
Identification Analysis of Fluid Type in the Low Resistivity Zone of Well Z-2 Field "Z", South Sumatera Sigit Rahmawan; Firman Herdiansyah; Suryo Prakoso; Muhammad Burhannudinnur; Syamsul Irham; Samsol; Muhammad Himawan Prakoso; Hayafa Fakhriyatul Ummah
Journal of Earth Energy Science, Engineering, and Technology Vol. 6 No. 2 (2023): JEESET VOL. 6 NO. 2 2023
Publisher : Penerbitan Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jeeset.v6i2.17522

Abstract

Hydrocarbon reserves are one of the main points that are very important in the sustainability of the productivity of an oil and gas field. This important point is greatly influenced by several parameters that can be obtained by various measurements and analysis. One of the most influential parameters in the analyses of the amount of hydrocarbon reserves in a reservoir is the water saturation value. The water saturation parameter will also be greatly influenced by the electrical parameters of the fluid-containing rock in the reservoir. Sometimes the electrical parameters of this rock, in this case resistivity becomes one of the benchmark parameters, whether the zone or reservoir has potential or is interesting to be developed or produced. However, there are several reservoirs or zones that experience low resistivity effects which will give an initial indication that the zones or reservoirs are not attractive or have no effect on development. In this Z field, there is a zone that experiences low resistivity effects, making this zone unattractive for production. So to be able to make these zones attractive for production, an identification analysis was carried out on Zones A and B in this Z field to determine the type or type of fluid from the two zones. The initial analysis was carried out petrographically from rock sample incisions at certain depths in Zones A and B so that it is known that the cause of the low resistivity effect in the two zones is the presence of pyrite minerals and illite clay which are the main causes of the low resistivity effect. Furthermore, an analysis of the identification of fluid types was carried out using the double apparent resistivity method with the results obtained that in Zones A and B there are 2 types of fluids, namely hydrocarbons and water with a depth limit of 3650 ft in Zone A and 4558 ft in Zone B. By knowing the type of fluid, the hydrocarbons contained in these two zones should be able to increase interest in the production of these zones as a potential zone for production, but it is necessary to perforate at a depth range indicated by the hydrocarbon fluid and carry out initial production tests to prove the results of the analysis in this study.
KARAKTERISTIK KESTABILAN LERENG DAERAH JATIGEDE KABUPATEN SUMEDANG, PROVINSI JAWA BARAT BERDASARKAN ANALISIS KINEMATIK Sofyan Rachman Idris; Dicky Muslim; Nana Sulaksana; M. Burhannudinnur
Jurnal Teknologi Mineral dan Batubara Vol 15 No 2 (2019): Jurnal Teknologi Mineral dan Batubara Edisi Mei 2019
Publisher : Balai Besar Pengujian Mineral dan Batubara tekMIRA

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30556/jtmb.Vol15.No2.2019.1009

Abstract

Daerah penelitian secara administratif berada di Kecamatan Jatigede, Kabupaten Sumedang, Provinsi Jawa Barat. Berdasarkan sudut pandang geologi, daerah Jatigede memiliki beberapa permasalahan yang timbul akibat kondisi geologi daerah tersebut yaitu berupa pengaruh keberadaan struktur geologi yang berhubungan dengan stabilitas maupun keruntuhan lereng. Untuk dapat mengidentifikasi tipe keruntuhan lereng batuan, dapat dilakukan analisis kinematik menggunakan metode scanline sampling. Penelitian ini dibagi menjadi 15 lokasi scanline sampling. Pada penelitian, dilakukan juga perhitungan uniaxial compressive strenght (UCS) dan rock quality designation (RQD) pada lereng tumpuan barat Bendungan Jatigede. Hasil analisis kinematik mendapatkan potensi tipe keruntuhan baji pada lereng scanline (SL) 1, 4 – 11 sedangkan pada lereng SL 2 dan 3 tidak memenuhi syarat keruntuhan baji serta didapatkan kualitas massa batuan (RQD) sedang-sangat baik serta penentuan nilai UCS yang menunjukan kekuatan material batuan yang lemah.
ANALISIS LINGKUNGAN PENGENDAPAN PADA LAPANGAN AR & RB FORMASI TALANG AKAR, CEKUNGAN SUMATRA SELATAN : ANALYSIS OF DEPOSIT ENVIRONMENT IN AR & RB FIELDS OF THE TALANG AKAR FORMATION, SOUTH SUMATRA Bramantyo, Andreas Rendy; Burhannudinnur, Muhammad; Koesmawardani, Wildan Tri
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.v4i2.16008

Abstract

Penelitian ini dilakukan pada lapangan AR & RB, formasi Talang Akar, Cekungan Sumatra Selatan. Dimana formasi Talang Akar ini memiliki potensi yang sangat besar dalam memiliki kandungan minyak bumi dan gas di Cekungan Sumatra Selatan ini, namun tidak semudah itu untuk menemukan minyak dan gas, perlu dilakukan analisis yang mendalam dalam melakukan eksplorasi. Salah satu analisis yaitu analisis lingkungan pengendapan. Dalam melakukan analisis ini menggunakan software petrel 2017. Berdasarkan hasil dari pengolahan data menghasilkan bahwa lapangan AR & RB terbentuk pada lingkungan pengendapan fluvial, delta plain dan delta front. Pembagian sekuen pada lapangan ARB terbagi menjadi 3 dan memiliki fasies yaitu flooding surface 1 terdapat fasies fluvial channel, point bar, creavase splay dan floodplain, flooding surface 2 terdapat fasies distributary channel, mouth bar dan mud flat dan flooding surface 3 terdapat fasies mouth bar dan mud flat. This research was conducted in field AR & RB, Talang Akar formation, South Sumatra Basin. Where the Talang Akar formation has enormous potential in containing oil and gas in the South Sumatra Basin, but did not find it to find oil and gas, in-depth analysis is needed to carry out exploration. One of the analyzes is the analysis of the depotitional environment. In conducting this analysis using petrel 2017 software. Based on the results of data processing, it was found that the AR & RB field was formed in a fluvial, delta plain and delta front environment. Sequence distribution in field ARB is divided into 3 and has facies, namely flooding surface 1 which has fluvial channel, point bar, creavase splay and floodplain facies, flooding surface 2 has distributed channel facies, mouth bar and mud flat and flooding surface 3 has mouth bar and mud flat facies.
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.
Utilization of Acoustic Wave Velocity for Permeability Estimation in Static Reservoir Modeling: A Field Case Prakoso*, Suryo; Burhannudinnur, Muhammad; Irano, Teddy; Herdiansyah, Firman
Aceh International Journal of Science and Technology Vol 10, No 1 (2021): April 2021
Publisher : Graduate School of Universitas Syiah Kuala

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13170/aijst.10.1.20328

Abstract

Several researches have shown that P-wave velocity carries information on the complexity of the rock's pore geometry and pore structure. Their complexity can be characterized by critical porosity. Therefore, the P-wave velocity is used to estimate permeability. This research uses data taken from the Tomori formation from Banggai-Sula basin, Central Sulawesi, which is a carbonate rock reservoir. Also, this research aims to obtain a 3D permeability model by using acoustic wave velocity cube data. The results show that permeability can be modeled well using acoustic wave velocity data. Furthermore, compared to the raw data log of permeability, the modeling results using wave velocity based on critical porosity show good results. This method is another alternative to permeability modeling if acoustic wave velocity cube data is available.
KARAKTERISTIK ALTERASI SKARN DAN DISTRIBUSI MINERAL SULFIDA PEMBAWA TEMBAGA DI TAMBANG BIG GOSSAN LEVEL 2860L-2940L FOOTWALL WEST, PAPUA, INDONESIA: CHARACTERISTICS OF SKARN ALTERATION AND SULPHIDE MINERAL BEARING COPPER DISTRIBUTION AT BIG GOSSAN MINE 2860L-2940L FOOTWALL WEST, PAPUA, INDONESIA Amalina, Nur; Meirawaty, Mira; Sonbait, Daniel; Burhannudinnur, Muhammad; Hafiz, Surya Darma; Rendy; Koesmawardani, Wildan Tri; Wijaya, Budi
Journal of Geoscience Engineering and Energy VOLUME 6, NOMOR 1, FEBRUARI 2025
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jogee.v6i1.22289

Abstract

Tambang Big Gossan di Papua Tengah dikenal dengan mineralisasi tembaga yang terbentuk akibat intrusi diorit pada batuan karbonatan Formasi Waripi. Penelitian ini bertujuan menganalisis karakteristik alterasi dan mineralisasi tembaga di level 2860, 2900, dan 2940 Footwall West. Metode yang digunakan termasuk pemetaan geologi dan analisis laboratorium (petrografi, mineragrafi, dan XRD). Hasilnya, ditemukan empat satuan litologi serta lima zona alterasi, yaitu klinopiroksen-garnet-kuarsa, epidot-klorit-kuarsa-kalsit, garnet-kuarsa-kalsit-piro pilit-epidot, piropilit-kuarsa-kalsit, dan aktinolit-kuarsa-klorit. Mineral sulfida tembaga utama adalah kalkopirit dan bornit, dengan pirit, pyrrhotite, dan magnetit sebagai mineral pembawa besi. Tembaga terakumulasi pada zona retrograde alterasi 2, 3, 4, dan 5. The Big Gossan mine in Central Papua is known for its copper mineralization, formed due to diorite intrusion into the carbonate rocks of the Waripi Formation. This study aims to analyze the characteristics of alteration and copper mineralization at levels 2860, 2900, and 2940 Footwall West. The methods used include geological mapping and laboratory analyses (petrography, mineragraphy, and XRD). The results revealed four lithological units and five alteration zones: clinopyroxene-garnet-quartz, epidote-chlorite-quartz-calcite, garnet-quartz-calcite-pyrophyllite-epidote, pyrophyllite-quartz-calcite, and actinolite-quartz-chlorite. The main copper sulfide minerals are chalcopyrite and bornite, with pyrite, pyrrhotite, and magnetite as iron-bearing minerals. Copper is concentrated in the retrograde alteration zones 2, 3, 4, and 5.
Potensi Pemanfaatan Air Danau Pascatambang di Wilayah Rumpin, Kabupaten Bogor, Jawa Barat Maulana, Yuga; Tuheteru, Edy Jamal; Burhannudinnur, Muhammad; Hartami, Pantjanita Novi; Suliestyah; Alan, Muhammad Rallupy Meyraldo
Jurnal Abdi Masyarakat Indonesia (JAMIN) Vol 6 No 2 (2024): JURNAL ABDI MASYARAKAT INDONESIA (JAMIN)
Publisher : Universitas Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25105/jamin.v6i2.18197

Abstract

Mineral and coal mining has a significant impact on the surrounding environment. One of these impacts is the formation of post-mining lakes, often referred to as mine voids or pit lakes. The unavailability of rocks or the lack of cover material to backfill the mining area forms post-mining lakes. A post-mining lake forms when water fills the mine hole. In rock mining with the quarry method that reaches a certain depth, post-mining lakes are often formed because all the rocks are taken as products, so that no cover rock remains. The existence of post-mining lakes in several areas can have both positive and negative impacts. The positive impact is the sustainable use of post-mining lakes, for example, as a water resource for the surrounding community. Given the important role of post-mining lakes, it is necessary to conduct socialization with the community about how to utilize them. One area that requires attention is the Rumpin area, Bogor Regency, West Java, which has many post-mining lakes. We expect the community to gain insight and input regarding the potential utilization of water from post-mining lakes through this socialization activity. Thus, we can achieve the goal of sustainable mining while directly benefiting the surrounding community.
Co-Authors Abdalrazaq, Eid Abdul Karim Adhitama, Ramadhan Alan, Muhammad Rallupy Meyraldo Albasri, A Anak Agung Sagung Mayun Yudhyasmara Prabandari Andreas Rendy Bramantyo Annisa Dewi Akbari, Annisa Dewi Arfiani Nur Arista Muhartanto Arista Muhartanto, Arista Asih Retno Dewanti Asraria, Dian Asseggaf, Abdurrahman Astri Rinanti Atridia Wilastrina Auliya, Hilyah Awang Eka Novia Rizali Bani Nugroho Bayu Satiyawira Benyamin Benyamin Benyamin Benyamin Benyamin Benyamin Benyamin, Benyamin Bramantyo, Andreas Rendy Budi Wijaya Cahaya Rosyidan Cahyaningratri Prima Riyandhani Choirunnisa, Hasna Ciptadhi Tri Oka Binartha Clara, Clara Dardji Noeradi Dicky Muslim Dwi Kurnianto Dyah Ayu Setyorini Eko Widianto Emelia Sari Erick Strada Dolok Saribu Fadliah, Fadliah Faisal Danu Tuheteru Filipus Armando Armando Ginting Firman Herdiansyah Firman Herdiansyah Firman Herdiansyah, Firman Galang Fahmi Maulana Ghanima Yasmaniar Gihon Nugrahadi Grace Khatrine Grace Stephani H Husna, H Hafiz, Surya Darma Hamid Nurrohman Hartami, Pantjanita Novi Hasri Hasri Havidh Pramadika Hayafa Fakhriyatul Ummah Hidayat, Hifdzan Rizki Himmes Fitra Yuda Husla, Ridha Imam Setiaji Ronoatmojo Indah Raya Irano, Teddy Ischak, Mohammad Junita Trivianty Musu Khatrine, Grace Koesmawardani, Wildan Tri Kollur, Shivaa Prasad Lestari Lestari Lukas Lukas Maman Djumantara, Maman Maulana, Galang Fahmi Maulana, Yuga Maulani, Mustamina Meirawaty, Mira Mixsindo Korra Herdyanti Mohamad Salsabila Mohammad Apriniyadi Mordekhai, Mordekhai Muhammad Himawan Prakoso Muhammad Yusril Ihza Mahendra Triany Mulia Ginting Mulia Ginting, Mulia Mustamina Maulani Musu, Junita Trivianty Nana Sulaksana Novi Triany Nugraheni, Rosmalia Dita Nur Amalina Onnie Ridaliani, Onnie Pantjanita Novi Hartami Paulina Taba Pearlo, Kevin Lukas Prakoso*, Suryo Putra, Raka Handika Ramadhan Adhitama Rendy Reno Pratiwi Reno Pratiwi Ricky Andrian Tampubolon Ririn Yulianti Ronoatmojo, Imam Setaiji Rosmalia Dita Nugraheni Rosmalia Dita Nugraheni Samsol Samsol Samura, Lisa Sangayu Ketut Laksemi Nilotama Saputra, Chaerudin Saribu, Erick Strada Dolok Setyorini, Dyah Ayu Shabrina Sri Riswati Sigit Rahmawan Soekardy, Mentari Gracia Sofyan Rachman Idris Sofyan Rachman, Sofyan Sonbait, Daniel Subandrio Sugiarto, Eddy Suherman Dwi Nuryana Suherman Dwi Nuryana Suliestyah Sulistiani Jarre Suryo Prakoso, Suryo Syahruddin Kasim Syamsul Irham Syamsul Irham Syavitri, Dewi Tampubolon, Ricky Andrian Teddy Irano Tuheteru, Edy Jamal Urbiyanto, Gemintang Atlantika Virginia Suryani Setiadi Wahid Wahab, Abdul Wegig Murwonugroho Widayati Putri, Tri wildan Tri K Wildan Tri Koesmawardani Wildan Tri Koesmawardani Wildan Tri Koesmawardani Yarra Sutadiwiria Yuda, Himmes Fitra Yudhyasmara Prabandari, Anak Agung Sagung Mayun Zahra, Audrey