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All Journal Prosiding Seminar Teknologi Kebumian dan Kelautan (SEMITAN Journal of Earth and Marine Technology (JEMT) Jurnal Abdi Masyarakat Indonesia Jurnal Geosaintek Eksplorium : Buletin Pusat Pengembangan Bahan Galian Nuklir
Sunan, Huzaely Latief
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Humanities Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Earth & Planetary Sciences Economics, Econometrics & Finance Education Energy Engineering Materials Science & Nanotechnology Physics Public Health Transportation

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The Relation of Fault Fracture Density with the Residual Gravity; case study in Muria Widiatmoko, Fajar Rizki; Putri, Ratih Hardini Kusuma; Sunan, Huzaely Latief
Journal of Earth and Marine Technology (JEMT) Vol 1, No 2 (2021)
Publisher : Lembaga Penelititan dan Pengabdian kepada Masyarakat - Institut Teknologi Adhi Tama Suraba

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jemt.2021.v1i2.1743

Abstract

The usages of the FFD analytical method massively are utilized during the last decade, especially in the geothermal preliminary study that can show the prospect reservoir area. This article discusses the correlation of the FFD value with the residual gravity value that is assumed as an indication of the underneath magmatic body. The correlation of FFD value with residual gravity value is applied in Muria mountain. Muria is classified as the volcano body that contains the magmatic body, also exist Genuk volcano and Patiayam hill around Muria. The correlation shows that FFD value and residual gravity value have a relation, but especially for the uninfluenced by structural activity has a low value of FFD. The correlation of FFD and residual gravity is double-checked with the ground truth data, it showing the proof relation. This way of methodology may use for finding the underneath magmatic body, especially applied to the surface that has not been influenced by structural activity.
TATANAN TEKTONIK BERDASARKAN POLA GEOKIMIA STUDI KASUS PADA GUNUNG KROMONG, CIREBON, JAWA BARAT Hadiyanto, Imam Fikri; Sunan, Huzaely Latief; Malik, Fikri Mahendra; Wildan, Dhofaeri; Oktaviani, Elvina; Gita P., Luh Ayu
Prosiding Seminar Teknologi Kebumian dan Kelautan Vol 3, No 1 (2021)
Publisher : Institut Teknologi Adhi Tama Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/p.semitan.2021.1975

Abstract

Pulau Jawa berada pada zona subduksi lempeng Indo-Australia dengan Eurasia. Aktivitas subduksi tersebut menghasilkan jajaran gunungapi (Vulcanic Arc), baik gunungapi aktif maupun gunungapi yang tidak aktif (gunungapi purba). Keberadaan gunungapi purba dapat menjadi salah satu petunjuk akan tatanan geotektonik yang terjadi pada masa lalu. Objek penelitian adalah Gunungapi Purba Kromong yang secara administratif termasuk ke dalam wilayah Kecamatan Ciwaringin, Kabupaten Cirebon, Provinsi Jawa Barat. Tujuan dari penelitian ini untuk mengetahui tatanan tektonik Gunungapi Purba Kromong berdasarkan pola geokimia batuan. Metode yang digunakan yaitu analisis petrografi untuk mengetahui komposisi batuan dan menentukan jenis litologi serta analisis geokimia batuan menggunakan metode XRF (X-Ray Flourescence) untuk menentukan tipe magma dan tatanan tektoniknya. Hasil analisis data geokimia batuan yang berdasarkan pada diagram ternary AFM (Alkali, Fe, dan Mg Oxides) menunjukan jenis magma Calc-Alcaline dan dari diagram geotektonik menunjukkan tatanan tektonik Island Arc. Berdasarkan penelitian ini dapat disimpulkan bahwa tatanan tektonik Gunungapi Purba Kromong termasuk ke dalam Island Arc hasil dari subduksi lempeng samudra dengan samudra.
PENGARUH SESAR PEGERSARI TERHADAP KEMUNCULAN INTRUSI MIKROGRANODIORIT DAERAH TULUNGAGUNG Sunan, Huzaely Latief; Pratomo, Septyo Uji; Eman, Brigita Nadya
Prosiding Seminar Teknologi Kebumian dan Kelautan Vol 3, No 1 (2021)
Publisher : Institut Teknologi Adhi Tama Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/p.semitan.2021.1966

Abstract

Struktur sesar umumnya membentuk retakan pada batuan sehingga bidang rekahan tersebut dapat menjadi bidang lemah bagi magma menuju ke permukaan dalam aktivitas magmatisme maupun vulkanisme. Lokasi penelitian yang terletak di Daerah Secang, Kecamatan Campurdarat, Kabupaten Tulungagung, Jawa Timur memiliki persebaran jalur sesar mendatar turun yang terdapat intrusi mikrogranodiorit di salah satu segmennya. Penelitian ini bertujuan untuk mengetahui pengaruh struktur geologi di lokasi penelitian terhadap keberadaan intrusi mikrogranodiorit. Penelitian ini menggunakan metode pemetaan geologi detail, analisis struktur geologi dan analisis petrografi. Stratigrafi lokasi penelitian dibagi menjadi enam satuan dari tua ke muda, yaitu Satuan Lava Andesit, Satuan Breksi Andesit, Satuan Intrusi Mikrogranodiorit, Satuan Breksi Polimik, Satuan Batugamping Terumbu, dan Satuan Aluvial. Hasil analisis data kekar di lapangan menunjukan sesar pagersari yang berarah barat daya - timur laut memiliki pergerakan mendatar mengiri (left strike-slip). Sesar pagersari membentuk struktur sesar penyerta berupa sesar pojok 1 dan sesar pojok 2 yang memotong satuan lava andesit dan breksi andesit. Hubungan potongmemotong dari hasil pemetaan dan analisis sesar menunjukkan sesar di lokasi penelitian terbentuk lebih dahulu dan intrusi mikrogranodiorit terbentuk kemudian. Kesimpulan dari urutan kejadian di lokasi penelitian bahwa sesar pagersari mempengaruhi pembentukan rekahan pada batuan sehingga menjadi jalur naiknya magma membentuk intrusi mikrogranodiorit.
Analysis of Tectonic Influence on Morphological Formation: Case Study of Gapura Pemalang Area Sunan, Huzaely Latief; Nurlatifah, Maula; Laksono, FX Anjar Tri; Widagdo, Asmoro
Journal of Earth and Marine Technology (JEMT) Vol 3, No 2 (2023)
Publisher : Lembaga Penelititan dan Pengabdian kepada Masyarakat - Institut Teknologi Adhi Tama Suraba

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jemt.2023.v3i2.4518

Abstract

Tectonic activity is closely related to the formation of landforms (morphology) in a region. The study area exhibits morphology controlled by normal fault tectonics, with blocks consisting of highlands and lowlands. This study aims to determine the extent of tectonic influence (normal faulting) on the morphology in the location. The quantitative geomorphological analysis method is used to obtain data on the level of tectonic activity present in the research area. Based on this method, it causes the formation of morphology and geological structures that affect the current surface forms. The methods used to calculate the tectonic influence are the Ratio of Valley Floor Width to Valley Height (Vf) and Mountain Front Sinuosity (Smf). Based on the results of the case study, the average Vf is 0.19, indicating class one tectonic activity and a high uplift level with V-shaped valleys. Meanwhile, the average Smf is 1.45, indicating strong tectonic activity associated with wide plains, narrow valleys, and steep hills. Based on these results, the study location falls into the category of strong tectonic activity, supported by field geological data showing right-lateral strike-slip faults and left-lateral normal faults intersecting each other.
The landscape formation history based on the detailed geological investigation in Aribaya and surrounding area, Pangetan district, Banjarnegara regency, Central Java Suranda, Annisa Helly; Sunan, Huzaely Latief; Permanajati, Indra
Journal of Earth and Marine Technology (JEMT) Vol 2, No 2 (2022)
Publisher : Lembaga Penelititan dan Pengabdian kepada Masyarakat - Institut Teknologi Adhi Tama Suraba

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jemt.2022.v2i2.2842

Abstract

The research site is in the Aribaya area and surrounding areas with an area of 16 km2 which is administratively included in Pagentan Subdistrict, Banjarnegara Regency, Central Java Province. The research area consists of 13 villages, namely: Suwidak, Pandansari, Karangtengah, Gumingsir, Karangnangka, Aribaya, Larangan, Talunamba, Clapar, Gununggiana, Pakelen, and Nagasari. Research objects in the form of Geomorphology, Stratigraphy, Geological Structure, Geological History, and Geological Potential. The geomorphology of the research area is divided into the Aribaya Fault Zone Unit, Gununnggiana Lava Flow Ridge Unit, and Aribaya Intrusion Unit. Based on unofficial lithostratigraphic units, the research area is divided into three rock units and the order from old to young, namely: Sandstone - Claystone Distribution Unit, Pyroclastic Brection Unit, and Diorit Intrusion Unit. Precipitated Sandstone - Claystone In the middle-upper neritic bathymetry environment, which belongs to the formation of the early Miocene – Middle-aged vines. Furthermore, tectonic activity occurs that causes the research area to form faults and syncline folds. Then at the time of the Early Pliocene, there was an influence from the activity of Mount Maung which provided sediment supply in the form of andesite fragments and matrix-sized Tuff Crystals so as to form a pyroclastic breccia unit. At the Time of the Pliocene, there was also diorite intrusion. The next process is the exogenous process that causes morphological form as it is today. The geological potential contained in the research area in the form of diorite mining excavations (positive potential) and landslide movement (negative potential) is quite a lot in the research area.
Kontrol Struktur Geologi pada Kemunculan Mata Air Panas Bumi di Daerah Subang, Jawa Barat Iswahyudi, Sachrul; Pamungkas, Muhamad Afirudin; Sunan, Huzaely Latief
Jurnal Geosaintek Vol. 5 No. 3 (2019)
Publisher : Institut Teknologi Sepuluh Nopember

Show Abstract | Download Original | Original Source | Check in Google Scholar

Abstract

Mata air panas Ciniru dan Subang terletak dibagian tenggara Gunung Ciremai, tepatnya terletak di Desa Subang, Kecamatan Subang, Kabupaten Kuningan, Jawa Barat. Terdapat 3 manifestasi panas bumi berupa mata air panas di Daerah Subang, yaitu 2 mata air panas di Daerah Ciniru dan 1 mata air panas Daerah Subang. Mata air panas Ciniru 1 keluar dari litologi batulempung, terdapat beberapa keluaran pada satu lokasi yang saling berdekatan, memiliki sinter travertin, rasa asin dan warna air berwarna coklat. Mata air panas Ciniru 2 keluar dari rekahan batuan yang terdapat di bawah tebing dengan litologi batupasir. Sedangkan mata air panas Subang keluar dari rekahan batupasir. Penelitian ini menggunakan metode pemetaan geologi, analisis anomali gaya berat, dan geokimia air mata air panas. Ketiga mata air panas terletak pada suatu kelurusan struktur geologi yang berarah relatif utara-selatan. Kehadiran stuktur geologi mengontrol kemunculan mata air panas di daerah penelitian. Beberapa struktur yang ditemukan adalah sesar mendatar kiri, sesar naik, dan lipatan sinklin dan antiklin. Berdasarkan analisis anomali residual dan geologi menunjukan perbedaan anomali yang signifikan yang kemudian diinterpretasikan sebagai daerah dengan litologi kompak batuan beku dengan densitas 2.8 - 3.1 gr/cm3; dan zona permeabel struktur geologi dengan densitas 1.97 - 2.6 gr/cm3. Ketiga manifestasi masuk dalam tipe air klorida, memiliki satu reservoir yang sama, memiliki temperature dari 136°C-159°C, dan tergolong sebagai sistem panas bumi temperatur sedang.
Manajemen Set Data Temperatur Packing Sealer di Pabrik Liquid Unilever Menggunakan Microsoft Power BI Kurniawan, Yogiek Indra; Chrismawan, Stephen Prasetya; Sunan, Huzaely Latief; Aditama, Maulana Rizki; Laksono, FX Anjar Tri
Jurnal Abdi Masyarakat Indonesia Vol 5 No 5 (2025): JAMSI - September 2025
Publisher : CV Firmos

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.54082/jamsi.2093

Abstract

Pabrik Liquid Unilever merupakan salah satu lini produksi yang memprioritaskan kualitas kemasan produk, khususnya jenis pouch, guna menghindari defect seperti kebocoran akibat temperatur penyegelan yang tidak optimal. Dalam upaya meningkatkan pemantauan kualitas kemasan, dilakukan Pengabdian Masyarakat yang bertujuan mengelola dan memvisualisasikan data temperatur mesin sealer menggunakan Microsoft Power BI. Data diperoleh dari sensor temperatur pada 21 mesin pengemasan dengan frekuensi pencatatan tinggi dan disimpan dalam file CSV secara berkala. Tahapan proyek meliputi pembersihan data (handling error, null, dan duplikasi), transformasi, pemodelan relasional, hingga pembuatan dashboard interaktif. Dashboard yang dikembangkan dilengkapi fitur filter berdasarkan tanggal, jenis mesin pouch, dan sensor temperatur (temp) sehingga memudahkan pengguna dalam menganalisis tren temperatur dan mengidentifikasi anomali yang dapat menyebabkan cacat kemasan. Evaluasi oleh mitra menunjukkan bahwa dashboard telah memenuhi kebutuhan pemantauan, meskipun performa pemuatan data masih perlu dioptimalkan. Proyek ini memberikan kontribusi nyata dalam pengambilan keputusan berbasis data di lini produksi serta dapat dikembangkan lebih lanjut melalui integrasi otomatisasi data dan fitur tambahan sesuai kebutuhan industri.
Interpretasi Struktur Geologi Berdasarkan Fault Fracture Density (FFD) dan Implikasinya Terhadap Potensi Likuefaksi di Daerah Kalibening, Kabupaten Banjarnegara, Jawa Tengah Sunan, Huzaely Latief; Gibran, Akhmad Khahlil; Aditama, Maulana Rizki; Iswahyudi, Sachrul; Widiatmoko, Fajar Rizki; Widagdo, Asmoro; Laksono, FX Anjar Tri
EKSPLORIUM Vol. 42 No. 1 (2021): MEI 2021
Publisher : BRIN Publishing

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17146/eksplorium.2021.42.1.6129

Abstract

The existence of geological structures is often associated with landslides and earthquakes. The Kalibening area is an interesting location for research on that purpose. This area is composed of Pleistocene and Recent rocks units. Based on its stratigraphy, the rocks in the area are truncated by fault structure. It means that the fault in the area is categorized as an active fault. The high morphology and a basin existence on its center indicate that the area formation was controlled by faults. The research is carried out to determine the trend of the geological structures that control the study area. To determine the trend of the geological structure, a structural mapping method of Fault Fracture Density (FFD) map combined with the Bouguer anomaly residual map and hillshade lineaments map is used. In general, the most important thing in the study of structural geology is the geometry of the structural elements. The conceptual model of geological structures is subsequently used to analyze the liquefaction potential of the study area. The interpretation of the structures shows the existence of dextral strike-slip fault followed by companion faults and pull-apart basin that is inferred as the result of normal faulting in the strike-slip mechanism. The dextral strike-slip fault produces a basin filled with loose sediment that is prone to liquefaction in the event of an earthquake and ground motion. This study concludes that the Kalibening area is prone to liquefaction due to the existence of the movement of dextral strike-slip fault, loose sediments that dominate the study area, and shallow groundwater table.
Co-Authors Aditama, Maulana Rizki Asmoro Widagdo, Asmoro Chrismawan, Stephen Prasetya Eman, Brigita Nadya Gibran, Akhmad Khahlil Gita P., Luh Ayu Hadiyanto, Imam Fikri Indra Permanajati, Indra Kurniawan, Yogiek Indra Laksono, FX Anjar Tri Malik, Fikri Mahendra Nurlatifah, Maula Oktaviani, Elvina Pamungkas, Muhamad Afirudin Pratomo, Septyo Uji Putri, Ratih Hardini Kusuma Sachrul Iswahyudi Suranda, Annisa Helly Widiatmoko, Fajar Rizki Wildan, Dhofaeri