GEOLOGI DAN DIAGENESA BATUGAMPING DAERAH WAYHELING DAN SEKITARNYA, KECAMATAN LENGKITI, KABUPATEN OKU, SUMATERA SELATAN

AKOYAMA, UMI and Setiawan, Budhi and Harnani, Harnani (2018) GEOLOGI DAN DIAGENESA BATUGAMPING DAERAH WAYHELING DAN SEKITARNYA, KECAMATAN LENGKITI, KABUPATEN OKU, SUMATERA SELATAN. Undergraduate thesis, Sriwijaya University.

	Text RAMA_34201_03071181320007.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (3MB) | Request a copy
Preview	Text RAMA_34201_03071181320007_0012117205_0001028404_01_front_ref.pdf - Accepted Version Available under License Creative Commons Public Domain Dedication. Download (716kB) | Preview
	Text RAMA_34201_03071181320007_0012117205_0001028404_02.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (381kB) | Request a copy
	Text RAMA_34201_03071181320007_0012117205_0001028404_03.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (266kB) | Request a copy
	Text RAMA_34201_03071181320007_0012117205_0001028404_04.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (825kB) | Request a copy
	Text RAMA_34201_03071181320007_0012117205_0001028404_05.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (560kB) | Request a copy
	Text RAMA_34201_03071181320007_0012117205_0001028404_06.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (182kB) | Request a copy
	Text RAMA_34201_03071181320007_0012117205_0001028404_07.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (106kB) | Request a copy
	Text RAMA_34201_03071181320007_0012117205_0001028404_08_ref.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (166kB) | Request a copy
	Text RAMA_34201_03071181320007_0012117205_0001028404_09_lamp.pdf - Accepted Version Restricted to Repository staff only Available under License Creative Commons Public Domain Dedication. Download (2MB) | Request a copy

Abstract

limestone of the area. The research method was carried out by geological mapping and analysis of the diagenetic environment through microscopic observations in sample aid samples. The Wayheling area is divided into three geomorphological units, namely the River andFloodl Plains (SDA), Steep Slope (PRDC), and the Lower Grounded Slope (PRDL). The stratigraphy of the study area is divided into three formations which are sorted from young keas, namely the Baturaja Formation which is ahead of the Early Miocene, the Gumai Formation which approaches the Middle Miocene, and the Kasai Formation which stands Pliocene. The geological structure that developed in the study area was in the form of stocky with Shear Fracture N 69 'E / 13, Gash Fracture N 355' E / 11, and direction of brecciation N 46 'E which showed a fault with the Normal Left Slip Fault type. Besides that, there are also five folded blades with Horizontal Upright Fold, Steeply Inclined Horizontal Fold, and Steeply Inclined Horizontal Fold. The structure shows the general direction of the Northwest- Southeast line which can be used in the order of Tertiary (Neogen) networks. Diagenetic products Limestone Wayheling area starts from the marine phreatic environment, which is characterized by microbial micritization and cementation of fibrous forms. Then the funeral environment marked with stylolite. Processes related to tectonics become mixing zones. After that, the meteoric phreaticic diagenesis was formed which was characterized by the formation of semen, then raised into a vadose environment which was marked by the presence of microcrystaline. The geological history of the study area begins with the formation of the Baturaja Formation and the Gumai Formation in harmony with the transgression phase at the time of the early Miocene-Middle Miocene. In the middle-end Miocene the deposition process was stopped because of the introduction of the regression phase which was carried out by the erosion process due to the raised part. In the Late Miocene-Pliocene developed

Item Type:	Thesis (Undergraduate)
Uncontrolled Keywords:	BATUGAMPING, Baturaja, Diagenesa
Subjects:	T Technology > TN Mining engineering. Metallurgy > TN400-580 Ore deposits and mining of particular metals
Divisions:	03-Faculty of Engineering > 34201-Geological Engineering (S1)
Depositing User:	Mr Halim Sobri
Date Deposited:	02 Oct 2019 06:42
Last Modified:	02 Oct 2019 06:42
URI:	http://repository.unsri.ac.id/id/eprint/10022

Actions (login required)

View Item