This project is about the study of carbonate sedimentology and structural geology of the limestone cliff face in Gunung Kanthan, Chemor, in Kinta Valley, Perak. The area is mostly made up of limestone hills that were remnants of massive carbonate beds covered with alluvial sediments and it has been mined by Lafarge Malayan Company. Due to the excavation and extraction of the limestone, the cliff face is now exposed and provides the opportunity to study the area. This research will provide geological study of the area as well as providing a geological map of the study area. The study is divided into two parts in which the first part is the geological mapping of the area followed by the relation of carbonate facies to the petrophysical proper...
The limestone of Tapak Formation is well exposed in the Ajibarang area and its surroundings, Central...
The Charu Formation of the Kuantan Group is exposed across the Sungai Lembing area in Pahang. This L...
The large scale of geological map (1: 750 000) does not give sufficient information about each outcr...
This project is about the study of carbonate sedimentology and structural geology of the limestone c...
This project is about the geology and economic potential of limestone in the Gunung Rapat area. The ...
This project is about the geology and economic potential of some carbonates rocks in the Gunung Kant...
Limestone hills are one of the significant features that can be found in Kinta Valley area. The lime...
This project is about the sedimentation and petrophysical characteristics of limestone found in Sung...
Gunung Kanthan limestone in Chemor, northern part of Kinta Valley, is part the massive Paleozoic Kin...
The limestone hills of the Kinta Valley are remnants of extensive limestone beds, which are part of ...
This project is about the sedimentation and petrophysical characteristics of limestone found in Sung...
The Kinta Valley area is surrounded by numerous limestone hills with numerous quarries operating for...
This research is about the geology and economic potential of Gunung Terendum area, Simpang Pulai. T...
This research focused on Thermal Maturation and Stratigraphy of the Black Shale Beds in the Kinta Li...
The ground mapping is done in order to produce 1:25,000 small scale of map which all the lithology i...
The limestone of Tapak Formation is well exposed in the Ajibarang area and its surroundings, Central...
The Charu Formation of the Kuantan Group is exposed across the Sungai Lembing area in Pahang. This L...
The large scale of geological map (1: 750 000) does not give sufficient information about each outcr...
This project is about the study of carbonate sedimentology and structural geology of the limestone c...
This project is about the geology and economic potential of limestone in the Gunung Rapat area. The ...
This project is about the geology and economic potential of some carbonates rocks in the Gunung Kant...
Limestone hills are one of the significant features that can be found in Kinta Valley area. The lime...
This project is about the sedimentation and petrophysical characteristics of limestone found in Sung...
Gunung Kanthan limestone in Chemor, northern part of Kinta Valley, is part the massive Paleozoic Kin...
The limestone hills of the Kinta Valley are remnants of extensive limestone beds, which are part of ...
This project is about the sedimentation and petrophysical characteristics of limestone found in Sung...
The Kinta Valley area is surrounded by numerous limestone hills with numerous quarries operating for...
This research is about the geology and economic potential of Gunung Terendum area, Simpang Pulai. T...
This research focused on Thermal Maturation and Stratigraphy of the Black Shale Beds in the Kinta Li...
The ground mapping is done in order to produce 1:25,000 small scale of map which all the lithology i...
The limestone of Tapak Formation is well exposed in the Ajibarang area and its surroundings, Central...
The Charu Formation of the Kuantan Group is exposed across the Sungai Lembing area in Pahang. This L...
The large scale of geological map (1: 750 000) does not give sufficient information about each outcr...