Udemy – Learn Sedimentology From The Scratch

What you'll learn
Students will learn about sedimentary structures, flow regimes
Primary sedimentary structures
Secondary sedimentary structures
Basin evolution & Analysis
Sedimentary Environments
Bouma Sequence
Sedimentary Textures
Requirements
Basics of Sedimentology
Flow regimes, Sedimentary structures
Basin Analysis
Basin Evolution
Description
Sedimentology, scientific discipline that is concerned with the physical and chemical properties of sedimentary rocks and the processes involved in their formation, including the transportation, deposition, and lithification (transformation to rock) of sediments. The objective of much sedimentological research is the interpretation of ancient environmental conditions in sediment source areas and depositional sites. Sedimentologists study the constituents, textures, structures, and fossil content of the deposits laid down in different geographic environments. By these means they can differentiate between continental, littoral, and marine deposits of the geologic record. Importance of sedimentary rocks.Sedimentary rocks provide a multitude of products which modern and ancient society has come to utilise.Art: marble, although a metamorphosed limestone, is an example of the use of sedimentary rocks in the pursuit of aesthetics and artArchitectural uses: stone derived from sedimentary rocks is used for dimension stone and in architecture, notably slate, a meta-shale, for roofing, sandstone for load-bearing buttressesCeramics and industrial materials: clay for pottery and ceramics including bricks; cement and lime derived from limestone.Economic geology: sedimentary rocks host large deposits of SEDEX ore deposits of lead-zinc-silver, large deposits of copper, deposits of gold, tungsten, Uranium, and many other precious minerals, gemstones and industrial minerals including heavy mineral sands ore depositsEnergy: petroleum geology relies on the capacity of sedimentary rocks to generate deposits of petroleum oils. Coal and oil shale are found in sedimentary rocks. A large proportion of the world's uranium energy resources are hosted within sedimentary successions.Groundwater: sedimentary rocks contain a large proportion of the Earth's groundwater aquifers. Our understanding of the extent of these aquifers and how much water can be withdrawn from them depends critically on our knowledge of the rocks that hold them (the reservoir).
Overview
Section 1: Sedimentology
Lecture 1 Sedimentary Structures - Part 1
Lecture 2 Sedimentary Structures - Part 2
Lecture 3 Sedimentary Structures - Part 3
Lecture 4 Conglomerate Types
Lecture 5 Clastic Rocks Classification
Lecture 6 Diagenesis, Lithification & Cements
Lecture 7 Deep Marine Environment
Lecture 8 Porosity and Permeability
Lecture 9 Buoma Sequence
Lecture 10 Classification Of Stylolites.
Lecture 11 Basin Analysis
Lecture 12 Reynolds, Froude number & Grain Size Scales
Lecture 13 Sphericity Numericals.
Lecture 14 Lagoons, Sedimentary Textures
Lecture 15 Transitional Sedimentary Environments.
Lecture 16 Dolomitisation and Terms related to Carbonate Classification.
Lecture 17 Sanstone Questions & Clastic Rock Classification
Lecture 18 Sedimentary Environments.
Lecture 19 Secondary Sedimentary Structures
All the Geology Students and those preparing for College, University and other Competitive exams.,UPSC, State PSC's and various other exams.

Homepage

https://www.udemy.com/course/learn-sedimentology-from-the-scratch/

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