for Journals by Title or ISSN
for Articles by Keywords
help

Publisher: UIN Maulana Malik Ibrahim Malang   (Total: 9 journals)   [Sort by number of followers]

Showing 1 - 9 of 9 Journals sorted alphabetically
CAUCHY     Open Access   (Followers: 1)
el-Hayah     Open Access  
El-Hikmah     Open Access   (Followers: 2)
EL-MUHASABA     Open Access   (Followers: 1)
J. de Jure     Open Access   (Followers: 2)
Jurnal NEUTRINO     Open Access  
LiNGUA : Jurnal Ilmu Bahasa dan Sastra     Open Access   (Followers: 2)
MADARASAH Jurnal Pendidikan dan Pembelajaran Dasar     Open Access  
MATICS     Open Access   (Followers: 1)
Journal Cover Jurnal NEUTRINO
  [0 followers]  Follow
    
  This is an Open Access Journal Open Access journal
   ISSN (Print) 1979-6374
   Published by UIN Maulana Malik Ibrahim Malang Homepage  [9 journals]
  • Back Matter

    • Authors: Kusairi S.Si
      Pages: 1 - 7
      PubDate: 2016-10-31
      Issue No: Vol. 9, No. 1 (2016)
       
  • INTERPRETATION OF BOUGUER ANOMALY TO DETERMINE FAULT AND SUBSURFACE
           STRUCTURE AT BLAWAN-IJEN GEOTHERMAL AREA

    • Authors: Anjar Pranggawan Azhari, Sukir Maryanto, Arief Rachmansyah
      Pages: 1 - 9
      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).
      PubDate: 2016-10-31
      Issue No: Vol. 9, No. 1 (2016)
       
  • HYPOCENTER DISTRIBUTION OF LOW FREQUENCY EVENT AT PAPANDAYAN VOLCANO

    • Authors: Muhammad Mifta Hasan, Hetty Triastuty, Bagus Jaya Santosa, Amien Widodo
      Pages: 19 - 23
      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.
      PubDate: 2016-10-31
      Issue No: Vol. 9, No. 1 (2016)
       
  • SEISMIC FACIES ANALYSIS ON 2D SEISMIC REFLECTION PROFILE IN “BARUNA”
           AND “JAYA” LINE AT NORTH EAST JAVA BASIN

    • Authors: Taufan Wiguna, Rahadian Rahadian, Sri Ardhyastuti, Safira Rahmah, Tati Zera
      Pages: 24 - 28
      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.
      PubDate: 2016-10-31
      Issue No: Vol. 9, No. 1 (2016)
       
  • SINGLE CHANNEL SEISMIC APPLICATION FOR GAS CHARGED SEDIMENT RECONNAISSANCE
           IN GEOHAZARD STUDY OF PORT CONSTRUCTION AT WETLAND AREA

    • Authors: Taufan Wiguna, Omar Moefti, Rahadian Rahadian, Muhamad Irfan
      Pages: 29 - 34
      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. 
      PubDate: 2016-10-31
      Issue No: Vol. 9, No. 1 (2016)
       
 
 
JournalTOCs
School of Mathematical and Computer Sciences
Heriot-Watt University
Edinburgh, EH14 4AS, UK
Email: journaltocs@hw.ac.uk
Tel: +00 44 (0)131 4513762
Fax: +00 44 (0)131 4513327
 
Home (Search)
Subjects A-Z
Publishers A-Z
Customise
APIs
Your IP address: 54.167.191.50
 
About JournalTOCs
API
Help
News (blog, publications)
JournalTOCs on Twitter   JournalTOCs on Facebook

JournalTOCs © 2009-2016