cover
Article Per Year (5 Year)
All
Home Page
OAI Link
Editorial Team
Contact
Reviewer
Google Scholar
Contact Name
Muhammad Kurniawan Alfadli
Contact Email
m.kurniawan@unpad.ac.id
Phone
+6285669298592
Journal Mail Official
bsc.ftg@unpad.ac.id
Editorial Address
-
Location
Kota bandung,
Jawa barat
INDONESIA
Bulletin of Scientific Contribution : Geology
Published by Universitas Padjadjaran
ISSN : 16934873     EISSN : 2541514X     DOI : doi.org/10.24198/bsc%20geology.v18i1
Core Subject : Science, Social, Engineering,
Civil Engineering, Building, Construction & Architecture Earth & Planetary Sciences Energy Environmental Science
BSC Geology adalah jurnal yang dikelola oleh Fakultas Teknik Geologi Universitas Padjadjaran,terbit 3 kali dalam setahun (April, Agustus, dan Desember), yang menerbitkan karya tulis ilmiah dalam bidang kebumian terutama yang berkaitan dengan geologi seperti : Petrologi Paleontologi Geomorfologi Stratigrafi Geologi Dinamik Geologi Lingkungan dan Hidrogeologi Geologi Teknik Geokimia Geofisika Sedimentologi. Setiap artikel yang akan diterbitkan adalah bersifat tanpa biaya (no processing charges dan no submission charges). Dewan redaksi dan penerbit tidak pernah meminta bayaran untuk penerbitan pada jurnal ini. Tujuan dari jurnal ini adalah untuk memperkaya pengetahuan dan informasi tentang ilmu kebumian dan dapat dimanfaatkan untuk kemaslahatan bersama.
Arjuna Subject : Ilmu Bumi dan Planet (semua kategori) - Geologi
Articles 6 Documents
 1 
Search results for , issue "Vol 6, No 2 (2008): Bulletin of Scientific Contribution" : 6 Documents clear
POTENSI BIJI BESI DI DAERAH AMBULANGAN, BANJAR, KALIMANTAN SELATAN Sunarie, Cecep Yandri
Bulletin of Scientific Contribution Vol 6, No 2 (2008): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (867.073 KB) | DOI: 10.24198/bsc.v6i2.8164

Abstract

Research area is located in Ambulangan, Banjar regency of South Kalimantan province. The research is aimed to indentified and mineral inventory of Iron Ore deposit, as well as primary or secondary type ore deposit. Morphology of the area is generally covered by hilly volcanic terrain with elevation below 650 m above sea level, the drainage pattern is mainly sub-parallel.Litology of the study area is covered mainly by Cretaceous rocks consists of Sediment, volcanic and andesitic intrusion.The iron ore occurred as primary and secondary type deposit. The primary type is exposing as vein like structure of approximately 6 m width and 50 m long, where as the secondary type is exhibiting as boulder or lateritic soil. Chemical analysis of primary iron ore indicated the ore grade is about 66.37% and 62.99% for secondary iron ore.
KONTROL STRUKTUR GEOLOGI TERHADAP SEBARAN BATUBARA DI DAERAH MENUKUNG-NANGAPINOH KALIMANTAN BARAT -, Iyan Haryanto
Bulletin of Scientific Contribution Vol 6, No 2 (2008): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (984.31 KB) | DOI: 10.24198/bsc.v6i2.8165

Abstract

Coal outcrop in Menukung area and Nangapinoh met in Melawi basin. This basin have experienced of several tectonic causes coal seam folded and faulted.Result of measurement entire coal outcrop shown strike between N 240°E – N 315°E with dip between 5° until 10°. Based on contruction result strike pattern known distribution coal in surface with orientation Southwest-Northeast and dip orientation Northwest, North until Northeast.dengan demikian sebaran batubara controlled by homocline fold structure. Based on strike and dip data and kind of geology structure that controlling it, so that known in northern research area have potention good enough.
THE INFLUENCE OF GEOMORPHOLOGY TO LANGUAGE VARIATION IN THE WESTERN PART OF JAVA, INDONESIA -, Evi Haerani; -, Dicky Muslim
Bulletin of Scientific Contribution Vol 6, No 2 (2008): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (205.959 KB) | DOI: 10.24198/bsc.v6i2.8161

Abstract

In Indonesia, the western part of Java Island is known as a place with very diverse culture. There are 3 provinces in this region, namely West Java, Banten, and Jakarta Capital Special Region with more than 40 million populations. Sundanese is a main culture within this region, where focal area is around Bandung City. It is accompanied by 3 other subcultures, i.e. Cirebonese (around Cirebon City), Betawinese (Jakarta City and surrounding) and Bantenese (around Serang City).Geomorphological configuration of the study area is characterized by mountainous to coastal plain areas. It implies to the characteristic diversity of culture for every community including the development of local languages. This paper is aimed to map the relationship of local languages diversity (dialect) with their geomorphological conditions in the study area.Result of the study shows that Sundanese people commonly speak humble in polite manner and live on mountainous to hilly area. The Cirebonese speaks rather Javanese combined with impolite Sundanese and lives on the northern Java coastal plain as transition area between Sundanese and Javanese. Betawinese speak rather impolite and live on the coastal plain around Gulf of Jakarta. Bantenese speak rather impolite and live on coastal plain to gentle hilly area. This result suggests that there is relationship between the characteristics of utterances of people with the nature they live on.
POTENSI GEOWISATA KAWASAN GUNUNG BADAK, TELUK CILETUH-SUKABUMI -, Mega F. Rosana
Bulletin of Scientific Contribution Vol 6, No 2 (2008): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (985.16 KB) | DOI: 10.24198/bsc.v6i2.8166

Abstract

Gunung Badak area, Ciletuh Bay, Sukabumi is area that has a rare diversity of rock at West Java region. Morphology of this area is interesting enough for one of the aspects of tourism, especially geological asptect (geotourism).This reveals the general geotourism potential in the Ciletuh Bay area. Method used in this study is a survey directly in the field and a review of some aspects of the geological literature Ciletuh. There are three groups of objects geotourism that can be developed in this area, namely: Amphiteater Morphology of Ciletuh Bay; Mandra Island; Manuk Island; Kunti Island and Lava pillows; G. Badak and G. Aseupan.Management and effective supervision are required to develop this potential to be geotourism, considering this area is part of Nature Reserve Cibanteng. Development potential to the south towards Ujung Genteng geotourism quite well developed for tourism towards the coast, and the green turtle protection.
GEOLOGI DAN ANALISIS TEKTONIK DAERAH KAMPAR SUMATRA TENGAH -, Faizal Muhamadsyah; -, Iyan Haryanto
Bulletin of Scientific Contribution Vol 6, No 2 (2008): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (736.953 KB) | DOI: 10.24198/bsc.v6i2.8162

Abstract

Central Sumatera basin controlled by an amount of regional stike-slip fault (wrench fault) moving on transtensinal system. Overall srike-slip pattern forming as negative flower structure, yielding horst and garben. This tecotonic process happened in Early Miocene.Graben forming begin the sedimentation process which indicate the coarse clastica deposit existence that goes on fluvial environment. This deposit equivalent with Sihapas formation that have an age of Eosen. The Sedimentary basin had a subsidence continuously till Middle of Miocene, that indicated by developt marine sedimentary rock.In Plio-Pleistocene, the uplifting processes is happen again that cause forming of fold and fault structure. Tectonic compression cause the research area more shallow and then become a continent. This is indicated by developted conglomerate, sandy conglomerate, tuffaceous sandstone which forming in continent.
EKSPLORASI BIJIH BESI DENGAN METODE DIPOLE-DIPOLE DAN GEOMAGNET DI WILAYAH GANTUNG, KABUPATEN BLITUNG TIMUR, PROVINSI BLITUNG -, Andi Agus Noor
Bulletin of Scientific Contribution Vol 6, No 2 (2008): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1217.238 KB) | DOI: 10.24198/bsc.v6i2.8163

Abstract

The geological distribution of iron ore in the area of research is relatively east-west with the thickness varies between 3-10 meters. Configuration subsurface geology of the results obtained with the method of exploration geophysics dipole-dipole and geomagnet.From the results of the exploration can be concluded that the distribution of iron ore almost evenly in all the track in the depth of 20 - 30 meters

Page 1 of 1 | Total Record : 6

 1 

Filter by Year

2008 2008


Reset
Filter By Issues
All Issue Vol 23, No 3 (2025): Bulletin of Scientific Contribution : GEOLOGY Vol 23, No 2 (2025): Bulletin of Scientific Contribution : GEOLOGY Vol 23, No 1 (2025): Bulletin of Scientific Contribution : GEOLOGY Vol 22, No 3 (2024): Bulletin of Scientific Contribution : GEOLOGY Vol 22, No 2 (2024): Bulletin of Scientific Contribution:GEOLOGY Vol 22, No 1 (2024): Bulletin of Scientific Contribution : GEOLOGY Vol 21, No 3 (2023): Bulletin of Scientific Contribution : GEOLOGY Vol 21, No 2 (2023): Bulletin of Scientific Contribution : GEOLOGY Vol 21, No 1 (2023): Bulletin of Scientific Contribution : GEOLOGY Vol 20, No 3 (2022): Bulletin of Scientific Contribution : GEOLOGY Vol 20, No 2 (2022): Bulletin of Scientific Contribution : GEOLOGY Vol 20, No 1 (2022): Bulletins of Scientific Contribution : Geology Vol 19, No 3 (2021): Bulletins of Scientific Contribution : Geology Vol 19, No 2 (2021): Bulletins of Scientific Contribution : Geology Vol 19, No 1 (2021): Bulletin of Scientific Contribution : GEOLOGY Vol 18, No 3 (2020): Bulletin of Scientific Contribution : GEOLOGY Vol 18, No 2 (2020): Bulletin of Scientific Contribution : GEOLOGY Vol 18, No 1 (2020): Bulletin of Scientific Contribution : GEOLOGY Vol 17, No 3 (2019): Bulletin of Scientific Contribution : GEOLOGY Vol 17, No 2 (2019): Bulletin of Scientific Contribution : GEOLOGY Vol 17, No 1 (2019): Bulletin of Scientific Contribution GEOLOGY Vol 16, No 3 (2018): Bulletin of Scientific Contribution GEOLOGY Vol 16, No 2 (2018): Bulletin of Scientific Contribution GEOLOGY Vol 16, No 1 (2018): Bulletin of Scientific Contribution GEOLOGY Vol 15, No 3 (2017): Bulletin of Scientific Contribution:GEOLOGY Vol 15, No 2 (2017): Bulletin of Scientific Contribution GEOLOGY Vol 15, No 1 (2017): Bulletin of Scientific Contribution Vol 14, No 3 (2016): Bulletin of Scientific Contribution Vol 14, No 2 (2016): Bulletin of Scientific Contribution Vol 14, No 1 (2016): Bulletin of Scientific Contribution Vol 13, No 3 (2015): Bulletin of Scientific Contribution Vol 13, No 2 (2015): Bulletin of Scientific Contribution Vol 13, No 1 (2015): Bulletin of Scientific Contribution Vol 12, No 3 (2014): Bulletin of Scientific Contribution Vol 12, No 2 (2014): Bulletin of Scientific Contribution Vol 12, No 1 (2014): Bulletin of Scientific Contribution Vol 11, No 3 (2013): Bulletin of Scientific Contribution Vol 11, No 2 (2013): Bulletin of Scientific Contribution Vol 11, No 1 (2013): Bulletin of Scientific Contribution Vol 10, No 2 (2012): Bulletin of Scientific Contribution Vol 10, No 1 (2012): Bulletin of Scientific Contribution Vol 9, No 3 (2011): Bulletin of Scientific Contribution Vol 9, No 2 (2011): Bulletin of Scientific Contribution Vol 9, No 1 (2011): Bulletin of Scientific Contribution Vol 8, No 3 (2010): Bulletin of Scientific Contribution Vol 8, No 2 (2010): Bulletin of Scientific Contribution Vol 8, No 1 (2010): Bulletin of Scientific Contribution Vol 7, No 2 (2009): Bulletin of Scientific Contribution Vol 7, No 1 (2009): Bulletin of Scientific Contribution Vol 6, No 2 (2008): Bulletin of Scientific Contribution Vol 6, No 1 (2008): Bulletin of Scientific Contribution Vol 5, No 3 (2007): Bulletin of Scientific Contribution Vol 5, No 2 (2007): Bulletin of Scientific Contribution Vol 5, No 1 (2007): Bulletin of Scientific Contribution Vol 4, No 2 (2006): Bulletin of Scientific Contribution Vol 4, No 1 (2006): Bulletin of Scientific Contribution Vol 3, No 2 (2005): Bulletin of Scientific Contribution More Issue