cover
Article Per Year (5 Year)
All
Home Page
OAI Link
Editorial Team
Contact
Reviewer
Google Scholar
Contact Name
Kusairi
Contact Email
kusairi@uin-malang.ac.id
Phone
-
Journal Mail Official
neutrino@uin-malang.ac.id
Editorial Address
-
Location
Kota malang,
Jawa timur
INDONESIA
Jurnal Neutrino : jurnal fisika dan aplikasinya
Published by Universitas Islam Negeri Maulana Malik Ibrahim Malang
ISSN : 19796374     EISSN : 24605999     DOI : -
Core Subject : Science,
Physics
Jurnal NEUTRINO (ISSN:1979-6374 / EISSN:2460-5999) adalah jurnal fisika yang dikelola dan diterbitkan oleh Jurusan Fisika Fakultas Sains Dan Teknologi Universitas Islam Negeri (UIN) Maulana Malik Ibrahim Malang. Jurnal NEUTRINO ini menjadi media bagi para akademisi dan praktisi untuk mengembangkan bidang fisika dan aplikasinya. Disamping itu Jurnal NEUTRINO bisa dijadikan sebagai media komunikasi ilmiah antar fisikawan baik di Indonesia juga seluruh dunia. Jurnal NEUTRINO memuat kajian-kajian fisika baik kajian teoritik, hasil eksperimen dan aplikasinya seperti fisika material, instrumentasi, komputasi, biofisika, fisika medis, fisika lingkungan, fisika teori, fisika nuklir, geofisika, elektronika, optika dan energi terbarukan. Jurnal NEUTRINO terbit 2 (dua) kali dalam setahun (April dan Oktober).
Arjuna Subject : -
Articles 4 Documents
 1 
Search results for , issue "Vol 9, No 1 (2016): October" : 4 Documents clear
INTERPRETATION OF BOUGUER ANOMALY TO DETERMINE FAULT AND SUBSURFACE STRUCTURE AT BLAWAN-IJEN GEOTHERMAL AREA Azhari, Anjar Pranggawan; Maryanto, Sukir; Rachmansyah, Arief
Jurnal Neutrino Vol 9, No 1 (2016): October
Publisher : Department of Physics, Maulana Malik Ibrahim State Islamic University of Malang

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1341.356 KB) | DOI: 10.18860/neu.v9i1.3664

Abstract

Gravity survey has been acquired by Gravimeter Lacoste Romberg G-1035 at Blawan-Ijen geothermal area. It was a focusing study from previous research. The residual Bouguer anomaly data was obtain after applying gravity data reduction, reduction to horizontal plane, and upward continuation. Result of Bouguer anomaly interpretation shows occurrence of new faults and their relative movement. Blawan fault (F1), F2, F3, and F6 are normal fault. Blawan fault is main fault controlling hot springs at Blawan-Ijen geothermal area. F4 and F5 are oblique fault and forming a graben at Banyupahit River. F7 is reverse fault. Subsurface model shows that Blawan-Ijen geothermal area was dominated by the Ijen caldera forming ignimbrite (ρ1=2.670 g/cm3), embedded shale and sand (ρ2=2.644 g/cm3) as Blawan lake sediments, magma intrusion (ρ3=2.814 g/cm3 ρ7=2.821 g/cm3), andesite rock (ρ4=2.448 g/cm3) as geothermal reservoir, pyroclastic air fall deposits (ρ5=2.613 g/cm3) from Mt. Blau, and lava flow (ρ6=2.890 g/cm3).
HYPOCENTER DISTRIBUTION OF LOW FREQUENCY EVENT AT PAPANDAYAN VOLCANO Hasan, Muhammad Mifta; Triastuty, Hetty; Santosa, Bagus Jaya; Widodo, Amien
Jurnal Neutrino Vol 9, No 1 (2016): October
Publisher : Department of Physics, Maulana Malik Ibrahim State Islamic University of Malang

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (627.219 KB) | DOI: 10.18860/neu.v9i1.3655

Abstract

Papandayan volcano is a stratovolcano with irregular cone-shaped has eight craters around the peak. The most active crater in Papandayan is a Mas crater. Distribution of relocated event calculated using Geiger Adaptive Damping Algorithm (GAD) shows that the epicenter of the event centered below Mas crater with maximum rms 0.114. While depth of the hypocenter range between 0-2 km and 5-6 km due to activity of steam and gas.
SEISMIC FACIES ANALYSIS ON 2D SEISMIC REFLECTION PROFILE IN BARUNA AND JAYA LINE AT NORTH EAST JAVA BASIN Wiguna, Taufan; Rahadian, Rahadian; Ardhyastuti, Sri; Rahmah, Safira; Zera, Tati
Jurnal Neutrino Vol 9, No 1 (2016): October
Publisher : Department of Physics, Maulana Malik Ibrahim State Islamic University of Malang

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (444.049 KB) | DOI: 10.18860/neu.v9i1.3665

Abstract

Two dimension (2D) seismic profile of Baruna and Jaya lines at North-East Java Basin show seismic reflector characteristics that can be used to interpret sediment thickness and continuity. Those reflector characteristics that can be applied for seismic facies analysis that represent depositional environment. This study starts from seismic data processing that using Kirchhoff Post Stack Time Migration method which is 2D seismic profile as result. Seismic reflector characterization has been done to both 2D profiles. Seismic reflector characterization was grouped as (i) individual reflection, (ii) reflection  configuration, (iii) reflection termination, (iv) external form. Individual reflection characteristics show high and medium amplitude, medium and low frequency, and continuous. Configuration reflection is continuous with parallel and subparallel type. Reflection termination shows onlap, and external form shows sheet drape. Local mound appearance can be interpreted as paleo-reef. Facies seismic anlysis result for this study area is shelf.
SINGLE CHANNEL SEISMIC APPLICATION FOR GAS CHARGED SEDIMENT RECONNAISSANCE IN GEOHAZARD STUDY OF PORT CONSTRUCTION AT WETLAND AREA Wiguna, Taufan; Moefti, Omar; Rahadian, Rahadian; Irfan, Muhamad
Jurnal Neutrino Vol 9, No 1 (2016): October
Publisher : Department of Physics, Maulana Malik Ibrahim State Islamic University of Malang

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (337.548 KB) | DOI: 10.18860/neu.v9i1.3666

Abstract

Gas charged sediment as a one of parameter for geohazard study in infrastructure especially in swamp area. Instability of sediment layer for exampel subsidence and landslide result in geohazard potention that caused by gas charged sediment. Seismic single channel can be used to identufy gas charged sediment location. Seabed morphology is collected from bathymetry and tidal survey. From seismic profile interpretation shows gas charged sediment indication in Line A and Line B. That indication emerged by presence of acoustic turbid zone and acoustic blanking. Line A and Line B location will be spotlight in next geotechnic port construction study. 

Page 1 of 1 | Total Record : 4

 1 

Filter by Year

2016 2016


Reset
Filter By Issues
All Issue Vol 18, No 1 (2025): October Vol 17, No 2 (2025): APRIL Vol 17, No 1 (2024): October Vol 16, No 2 (2024): APRIL Vol 16, No 1 (2023): October Vol 15, No 2 (2023): APRIL Vol 15, No 1 (2022): October Vol 14, No 2 (2022): APRIL Vol 14, No 1 (2021): October Vol 13, No 2 (2021): APRIL Vol 13, No 1 (2020): October Vol 12, No 2 (2020): April Vol 12, No 1 (2019): October Vol 11, No 2 (2019): April Vol 11, No 1 (2018): OCTOBER Vol 11, No 1 (2018): October Vol 10, No 2 (2018): April Vol 10, No 1 (2017): October Vol 9, No 2 (2017): April Vol 9, No 1 (2016): October Vol 8, No 2. APRIL (2016): JURNAL NEUTRINO Vol 8, No 1. Oktober (2015): JURNAL NEUTRINO Jurnal Neutrino (Vol.7 No. 2 JURNAL NEUTRINO (Vol 7, No 1 JURNAL NEUTRINO (Vol 6, No 2 JURNAL NEUTRINO (Vol 6, No 1 JURNAL NEUTRINO (Vol 5, No 2 JURNAL NEUTRINO (Vol 4, No 2 JURNAL NEUTRINO (Vol 4 No 1 JURNAL NEUTRINO (Vol 3 No 2 JURNAL NEUTRINO (Vol 3 No 1 JURNAL NEUTRINO (Vol 2 No 2 JURNAL NEUTRINO (Vol 2 No 1 JURNAL NEUTRINO (Vol 1 No 2 JURNAL NEUTRINO (Vol 1 No 1 More Issue