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PEMODELAN BAWAH PERMUKAAN BANTAR KARET, JAWA BARAT MENGGUNAKAN METODE GRAVITASI

JURNAL GEOCELEBES · Vol. 3 No. 2 (2019) · pp. 59–65

DOI
10.20956/geocelebes.v3i2.6689
ISSN
2579-5546, 2579-5821
Published
2019-10-03
Publisher
Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar
Language
en

Abstract

Gravity method is one of the geophysical methods that is often used to obtain information about the subsurface through differences density of the rocks around it. Gravity anomaly data used in this study is primary data that has been processed data. Data processing is obtained by reducing gravity observation data until complete bouguer anomaly values. The results of the interpretation of the gravity anomaly show that the types of rocks in subsurface of the study area are peridotite, tuff, riolite and basalt. The rock with the highest density is peridotite with a density value of 3.15 gr/cm3. This is due to the intrusion process to forming peridotite and there are two zones boundaries which have very significant density differences.

Collaboration network of the authors

40 authors · 85 co-authorship links · showing the 40 most connected

Hover or tap a name to highlight its co-authors. Double-click to open the author's page.

  • Universitas Halu Oleo
  • Universitas Muhammadiyah Kendari
  • Affiliation unknown
  • Different organisations
  • Same organisation
  • Affiliation unknown
  • Thicker line = more joint articles · bigger circle = more articles
Show as table
Co-authorOrganisationJoint articles
Emi Prasetyawati UmarAffiliation unknown7
Muhammad Fawzy Ismullah MassinaiAffiliation unknown2
Aryadi NurfalaqAffiliation unknown2
Erfan SyamsuddinAffiliation unknown2
Septian Tri NugrahaAffiliation unknown2
Asrul JayaUniversitas Halu Oleo1
La Ode Muh UmranAffiliation unknown1
La SensuUniversitas Halu Oleo1
Deity YuningsihUniversitas Halu Oleo1
Muhammad Sabaruddin SinapoyUniversitas Halu Oleo1
Indria HafizahAffiliation unknown1
Juminten SaiminAffiliation unknown1
Satrio WicaksonoAffiliation unknown1
Ashaeryanto AshaeryantoAffiliation unknown1
Amiruddin EsoUniversitas Halu Oleo1
Nur JanaAffiliation unknown1
Arimaswati ArimaswatiAffiliation unknown1
Andy Rafdi Al BagizAffiliation unknown1
Irawaty IrawatyUniversitas Halu Oleo1
Fercee PrimulaAffiliation unknown1
Wa Ode Sitti MusninaAffiliation unknown1
Yonelian YuyunAffiliation unknown1
M. Sulaiman ZubairAffiliation unknown1
Ritha PratiwiAffiliation unknown1
Budi BudiAffiliation unknown1
La BatiaUniversitas Halu Oleo1
Darman DarmanUniversitas Muhammadiyah Kendari1
Irwan GaniAffiliation unknown1
Suyuti SuyutiAffiliation unknown1
Muh JafarAffiliation unknown1
Musriady MusriadyAffiliation unknown1
Ahmad Rif'an Khoirul LisanAffiliation unknown1
Romuald SohoresAffiliation unknown1
Hasanuddin HasanuddinAffiliation unknown1
Wira SunaryaAffiliation unknown1
Syamsuddin SyamsuddinAffiliation unknown1

Affiliations come from OpenAlex; journal OAI-PMH metadata carries none. Authors without an OpenAlex ID are matched by name, which can merge or split people.

Metadata source: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/geocelebes/oai, first harvested 3 Nov 2026, last seen 3 Nov 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en">PEMODELAN BAWAH PERMUKAAN BANTAR KARET, JAWA BARAT MENGGUNAKAN METODE GRAVITASI</dc:title>
	<dc:creator xml:lang="en">Jamaluddin, Jamaluddin</dc:creator>
	<dc:creator xml:lang="en">Maria, Maria</dc:creator>
	<dc:creator xml:lang="en">Ryka, Hamriani</dc:creator>
	<dc:creator xml:lang="en">Afifah, Rohima Sera</dc:creator>
	<dc:description xml:lang="en">Gravity method is one of the geophysical methods that is often used to obtain information about the subsurface through differences density of the rocks around it. Gravity anomaly data used in this study is primary data that has been processed data. Data processing is obtained by reducing gravity observation data until complete bouguer anomaly values. The results of the interpretation of the gravity anomaly show that the types of rocks in subsurface of the study area are peridotite, tuff, riolite and basalt. The rock with the highest density is peridotite with a density value of 3.15 gr/cm3. This is due to the intrusion process to forming peridotite and there are two zones boundaries which have very significant density differences.</dc:description>
	<dc:publisher xml:lang="en">Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar</dc:publisher>
	<dc:date>2019-10-03</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.unhas.ac.id/index.php/geocelebes/article/view/6689</dc:identifier>
	<dc:identifier>10.20956/geocelebes.v3i2.6689</dc:identifier>
	<dc:source xml:lang="en">JURNAL GEOCELEBES; Vol. 3 No. 2: October 2019; 59-65</dc:source>
	<dc:source>2579-5546</dc:source>
	<dc:source>2579-5821</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/geocelebes/article/view/6689/4486</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2019 JURNAL GEOCELEBES</dc:rights>
</oai_dc:dc>