Latest Issue
Development of Eco-Friendly Microplastic Removal Filter For Sea Salt Farm
Published: August 31,2026Flood Modeling in the Lower Mekong Basin: A 2D Hydrodynamic Approach in Cambodia
Published: August 31,2026Monitoring Water Quality in Indoor Mud Crab (Scylla serrata) Farming Systems
Published: August 31,2026Development of Oyster Sauce Using Japanese Oysters, Green Mussels, and Clams
Published: August 31,2026Analysis of Pesticide Residues in Groundwater of Agriculturally Intensive Regions of Cambodia
Published: August 31,2026Development of Soy Sauce by Using Different Molds during Koji Fermentation
Published: August 31,2026Preliminary Investigation on Organic Petrology of Shale in Phnom Mrech, Angkor Chum District, Siemreap Province, Onshore Cambodia
-
1. Faculty of Chemical and Food Engineering, Institute of Technology of Cambodia, Russian Federation Blvd., P.O. Box 86, Phnom Penh, Cambodia.
Academic Editor:
Received: July 19,2021 / Revised: / Accepted: November 19,2021 / Available online: December 30,2021
The aim of this study is to investigate the organic petrology of shale in Phnom Mreach, Angkor Chum District, Siem Reap province, onshore Cambodia. Thin-section is carried out to analyze mineral compositions, sedimentary texture, and shale classification. Polish-section is used to identify the types of organic matter under reflected light. Scanning electron microscope (SEM) is analyzed for further detailed study on types and morphology of organic matter. The results showed that shales are mainly composed of quartz, clay minerals, calcite, mica, and small amount of plagioclase. Moreover, shales are classified into silica-rich argillaceous mudstone and clay-dominated lithotype. These shales consist of parallel and wavy lamina-structures. Furthermore, there are three types of organic matter are identified under SEM and polish section, such as vitrinite, inertinite, and alginite. Moreover, the organic petrology of shales can contribute to better understanding sources of organic matter. The presence of vitrinite and inertinite is suggested that organic matter has a source from woody tissues and plant materials that belong to a humic-type deposit.
