The Sriwijaya University Library

  • Home
  • Information
  • News
  • Help
  • Librarian
  • Login
  • Member Area
  • Select Language :
    Arabic Bengali Brazilian Portuguese English Espanol German Indonesian Japanese Malay Persian Russian Thai Turkish Urdu

Search by :

ALL Author Subject ISBN/ISSN Advanced Search

Last search:

{{tmpObj[k].text}}
Image of PETROGENESA BASAL FORMASI GARBA, DAERAH BUMI GENAP DAN SEKITARNYA, KABUPATEN OKU SELATAN, SUMATERA SELATAN

Skripsi

PETROGENESA BASAL FORMASI GARBA, DAERAH BUMI GENAP DAN SEKITARNYA, KABUPATEN OKU SELATAN, SUMATERA SELATAN

Rendiansyah, Muhammad - Personal Name;

Penilaian

0,0

dari 5
Penilaian anda saat ini :  

Garba Formation is located at the boundary of the South Sumatra Basin of Late Jurassic-Early Cretaceous age. This research was conducted in Bumi Genap area, South Ogan Komering Ulu Regency, South Sumatra Province. In the research area found basalt rocks that have various igneous structures and in petrographic analysis also found a variety of special textures. These geological conditions make this research area interesting to conduct further research, especially to explain how the formation of basalt rocks in the research area. In this study, 11 observation locations were analyzed both petrologically and petrographically. Based on petrological analysis, various kinds of igneous structures such as massive, vesicular, sheeting joint, columnar joint, flow structure, and pillow lava were obtained. While in the petrographic analysis of basalt rocks of the Garba Formation, several special textures were found such as intergranular, porphyritic, glomerophyric, hyalopilitic, pilotassitic, zoning, and sieve. The petrogenesis process begins when magma finally reaches the surface as lava and flows towards lower elevations where the lava flow undergoes cooling to form sheeting joint structures and flow structures. Lava that has not undergone cooling continues to flow towards lower elevations where the lava still contains trapped gas bubbles and later returns to cooling and forms vesicular and massive structures. During the cooling of the lava, there was concordant intrusion in the form of a sill which also experienced cooling to form sheeting joint and massive structures. As the cooling progresses, discordant intrusion in the form of dike occurs which forms a columnar joint structure. Magma continues to try to escape to the surface through the fracture gap so that it experiences direct contact with seawater suddenly and produces a pillow lava structure.


Availability
Inventory Code Barcode Call Number Location Status
2507001525T168301T1683012025Central Library (REFERENCES)Available but not for loan - Not for Loan
Detail Information
Series Title
-
Call Number
T1683012025
Publisher
Indralaya : Prodi Teknik Geologi, Fakultas Teknik Universitas Sriwijaya., 2025
Collation
xv, 39 hlm.; ilus.; tab.; 29 cm.
Language
Indonesia
ISBN/ISSN
-
Classification
551.07
Content Type
-
Media Type
-
Carrier Type
-
Edition
-
Subject(s)
Geologi
Prodi Teknik Geologi
Specific Detail Info
-
Statement of Responsibility
TUTI
Other version/related

No other version available

File Attachment
  • PETROGENESA BASAL FORMASI GARBA, DAERAH BUMI GENAP DAN SEKITARNYA, KABUPATEN OKU SELATAN, SUMATERA SELATAN
Comments

You must be logged in to post a comment

The Sriwijaya University Library
  • Information
  • Services
  • Librarian
  • Member Area

About Us

As a complete Library Management System, SLiMS (Senayan Library Management System) has many features that will help libraries and librarians to do their job easily and quickly. Follow this link to show some features provided by SLiMS.

Search

start it by typing one or more keywords for title, author or subject

Keep SLiMS Alive Want to Contribute?

© 2025 — Senayan Developer Community

Powered by SLiMS
Select the topic you are interested in
  • Computer Science, Information & General Works
  • Philosophy & Psychology
  • Religion
  • Social Sciences
  • Language
  • Pure Science
  • Applied Sciences
  • Art & Recreation
  • Literature
  • History & Geography
Icons made by Freepik from www.flaticon.com
Advanced Search