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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 8, No 1 (2010): Bulletin of Scientific Contribution" : 6 Documents clear
PENDIDIKAN GEOLOGI MILITER DI INDONESIA, SUATU TANTANGAN BAGI PUSDIKLAT GEOLOGI DAN PERGURUAN TINGGI PENYELENGGARA PENDIDIKAN SAINS KEBUMIAN -, Zufialdi Zakaria
Bulletin of Scientific Contribution Vol 8, No 1 (2010): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (226.103 KB) | DOI: 10.24198/bsc.v8i1.8244

Abstract

Geology plays a role in various fields. In the field of military and national defense, geological branch that play a role is military geology. In Indonesia, there are no special units of military geology that handling of military geology. Military geology education was also not in the curriculum of the University of geoscience education providers. Geological training and education center is also not have modules and syllabus for military geology . These conditions is a challenge to provide military-geology education for personnel of military of Indonesian National Army , or to the geologists who are interested in working in the military
HUBUNGAN ANTAR KOMPONEN MIKROFASIES LERENG TERUMBU DAN CEKUNGAN LOKAL BELAKANG TERUMBU PADA BATUGAMPING BIOKLASTIKA FORMASI BATURAJA DI DAERAH SEKITAR MUARADUA, SUMATERA SELATAN -, Sigit Maryanto
Bulletin of Scientific Contribution Vol 8, No 1 (2010): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1460.087 KB) | DOI: 10.24198/bsc.v8i1.8240

Abstract

Bioclastic limestones from Baturaja Formation cropped out at Muaradua area, South Sumatera is a good object of research for studying microfacies of limestone. Based on the rock features under the polarization microscope of the bioclastic limestones taking from studied area could be predicted the limestones are predominantly deposited at reef-flank and back-reef local basin. The main components T-F-P test of the limestones showing a significant difference of the carbonate grains, terrigenous grains, and neomorphism materials between two depositional environments. The other side, matrix, cement, and rock porosity components have no significant difference.
LITOSTRATIGRAFI CEKUNGAN OMBILIN BERDASARKAN INTERPRETASI CITRA SATELIT -, Yuyun Yuniardi
Bulletin of Scientific Contribution Vol 8, No 1 (2010): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1340.786 KB) | DOI: 10.24198/bsc.v8i1.8241

Abstract

Stratigraphy of Ombilin Basin area was interesting for make some research. The research did use remote sensing interpretation to made geological interpretation map which is containing information about lithostratigraphic unit distribution in Ombilin Basin area. LithoStratigraphic of Ombilin Basin from old to young were Brani Formation, Sangkarewang Formation, Sawahlunto Formation, Sawahtambang Formation, and Ombilin Formation.
PENGELOLAAN AIRTANAH YANG BERWAWASAN LINGKUNGAN OLEH INDUSTRI AIR MINUM DALAM KEMASAN (AMDK) -, T. Yan W. M. Iskandarsyah; -, Hendarmawan
Bulletin of Scientific Contribution Vol 8, No 1 (2010): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/bsc.v8i1.8242

Abstract

Sustainability of production of bottled drinking water is highly dependent and influenced by the condition of the recharge zone. Thus, knowledge and understanding of local conditions and the behavior of groundwater recharge to the springs is required. To get a decent source of water produced and minimize the impact can inflict negative, then P.T. Tirta Investama implemented several stages such as literature study, identifying the area, a preliminary survey, detail survey, EIA studies, the production (construction and installation), and recharge area study at least one year. Protection of water resources taken from the aquifer is not used by people around in general (aquifers) as well as against the source of water which is generally utilized by the population (unconfined aquifer) translated in the construction of a well borehole. Meanwhile, study catchment areas become the crucial factor in the management of groundwater, natural feedback input is one of the factors associated with the process of infiltration.From this study obtained distribution of the origin of groundwater (recharge) to the water that comes out (discharge) and the layers that tend vulnerable to groundwater contamination. Studies recharge area for a minimum of one year is a very important study as sustainable groundwater resource management efforts in order water balance in a region.
PENARIKHAN RADIOKARBON KAITANNNYA DENGAN DINAMIKA DAUR PROSES PENGENDAPAN KUARTER FLUVIAL DAN DANAU TERHADAP PERUBAHAN IKLIM DAN TEKTONIK DI PAPARAN DANAU SINGKARAK, KAB. SOLOK, SUMATERA BARAT -, Herman Mulyana; -, Herman Moechtar
Bulletin of Scientific Contribution Vol 8, No 1 (2010): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1102.141 KB) | DOI: 10.24198/bsc.v8i1.8243

Abstract

The Quaternary deposits in the studied area comprises of river channel, floodplain, swampy which influence by rising and falling of lake level, lake, tidal-lake, and swamp deposits. These deposited separated by three depositional intervals (IP I-III). Vertically, the character of environment changing seems not gradually. These differences caused by dominant of tectonic effects. Therefore, climate was not important force in controlling the change of the environments. It’s mean, the sedimentary processes on the basin were under controlled by tectonic.
PENURUNAN MUKA TANAH DI KOTA-KOTA BESAR PESISIR PANTAI UTARA JAWA (STUDI KASUS : KOTA SEMARANG) Sophian, Raden Irvan
Bulletin of Scientific Contribution Vol 8, No 1 (2010): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/bsc.v8i1.55904

Abstract

ABSTRACTMajor cities in the north coast of Java developed in estuarine watersheds.  Genetically, sediment material scattered in the region.  Sediments of  weathering and erosion result,  is carried by a river sediment in the river estuaries.  Characteristics of the material-forming region, is dependent upon the crushed rock by river. Phenomenon of subsidence / land subsidence occurred in this many areas. Naturally, these regions experiencing land subsidence resulting from sediment material properties. This subsidence can be caused by various factors, for example due to soil load itself, so there is a decrease naturally. Consolidation is  included in the normal consolidation. Factors considered in knowing subsidence, is a load of soil itself on each layer of fine-clastic, so that can be known susidence due to overburden load. Within a certain timeframe land subsidence is still going to happen, especially in the northern part of  Semarang city (old city) which can be resulted in a tide flood so that it must consider its handling.  Keywords: alluvial, land subsidence, consolidation, overburden, tide flood ABSTRAKKota-kota besar di pesisir pantai utara Jawa banyak berkembang di daerah muara aliran sungai. Secara genetik, di wilayah tersebut tersebar material endapan aluvial. Endapan-endapan hasil  pelapukan dan erosi terbawa oleh air sungai yang mengendap di muara sungai. Karakteristik material  penyusun wilayah sangat tergantung oleh batuan yang digerus oleh sungai tersebut. Fenomena amblesan/ penurunan muka tanah  banyak terjadi di wilayah ini. Secara alami, daerah tersebut mengalami penurunan muka tanah akibat dari sifat material endapan aluvial. Penyebab terjadinya penurunan ini dapat diakibatkan oleh berbagai faktor, salah satunya akibat beban tanah itu sendiri, sehingga terjadi penurunan secara alami. Konsolidasi yang terjadi termasuk ke dalam normal konsolidasi.  Faktor yang diperhitungkan untuk mengetahui penurunan yang terjadi, adalah beban tanah itu sendiri pada setiap  lapisan klastika halus, sehingga dapat diketahui penurunan akibat beban overburden. Dalam jangka waktu tertentu penurunan muka tanah masih akan terjadi, terutama di kota Semarang bagian utara (kota lama) yang dapat mengakibatkan terjadinya banjir laut pasang sehingga perlu dipikirkan penanggulangannya.        Kata kunci: aluvial, land subsidence, konsolidasi, overburden, banjir rob

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