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 STUDI STRATIGRAFI PADA FORMASI TALANG AKAR BERDASARKAN DATA PERMUKAAN DAERAH SUKOMORO DAN SEKITARNYA, KABUPATEN BANYUASIN

Skripsi

STUDI STRATIGRAFI PADA FORMASI TALANG AKAR BERDASARKAN DATA PERMUKAAN DAERAH SUKOMORO DAN SEKITARNYA, KABUPATEN BANYUASIN

Prakoso, Rio Bagas - Personal Name;

Penilaian

0,0

dari 5
Penilaian anda saat ini :  

The Sukomoro area and its surroundings, Banyuasin Regency, South Sumatera have characteristics of sedimentary rocks of late Oligocene to Early Miocene age which were deposited in the South Sumatera Basin and are included in the Talang Akar Formation, Gumai Formation, and Air Benakat Formation. The analysis process was carried out using the lithofacies analysis method (Mial, 1985) to determine the depositional environment. By classifying each type of lithofacies that has been obtained from the stratigraphic column into facies association groups. From the facies association data, it will produce data in the form of interpretation of the depositional environment in the study area. The results of data processing in the form of visualization in the form of a map of the depositional environment. The results of data processing in the form of visualization in the form of a map of the depositional environment. Based on the analysis of the stratigraphic column in the study area, 7 types of lithofacies were obtained, namely Litofacies (Sg), Litofacies (Sm), Litofacies (St), Litofacies (Sc), Litofacies (Sh), Litofacies (Fl), and Litofacies (Fsc). The facies association analysis of the Talang Akar Formation can be divided into four facies associations which are included in an intertidal tidal depositional system, namely tidal channel, tidal sand flat, tidal sand-mud mixed flat, and tidal mud flat. The Talang Akar Formation can be interrupted was deposited in the transition zone starting from intertidal-subtidal.


Availability
Inventory Code Barcode Call Number Location Status
2207003063T76788T767882022Central Library (Referens)Available
Detail Information
Series Title
-
Call Number
T767882022
Publisher
Indralaya : Prodi Teknik Geologi, Fakultas Teknik Universitas Sriwijaya., 2022
Collation
x, 54 hlm.; ilus.; 29 cm
Language
Indonesia
ISBN/ISSN
-
Classification
552.207
Content Type
Text
Media Type
-
Carrier Type
-
Edition
-
Subject(s)
Formasi Talang Akar
Teknik Geologi
Specific Detail Info
-
Statement of Responsibility
MURZ
Other version/related

No other version available

File Attachment
  • Mengambil data. Tunggu beberapa detik dan cobalah memotong atau menyalin lagi.
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