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Learn Sedimentology from the Scratch
Rating: 4.2 out of 5(14 ratings)
233 students

Learn Sedimentology from the Scratch

Petrology: Sedimentology & Basin Analysis
Created byJohn Martin
Last updated 12/2021
English
English [Auto],

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

Course content

1 section19 lectures20h 24m total length
  • Sedimentary Structures - Part 11:09:21

    Discover sedimentary structures and textures, classify primary, secondary, inorganic, and organic types, and identify top, bottom, and within-bed features like ripple marks and desiccation cracks to infer deposition.

  • Sedimentary Structures - Part 21:10:20

    Explore sedimentary structures formed within beds, including mud cracks and desiccation features, model X and pseudo structures, cross-bedding types, lenticular bedding, and related stratification patterns.

  • Sedimentary Structures - Part 31:21:51

    Learn about bottom sedimentary structures, or sole marks, formed by erosional and depositional processes, and identify directional indicators like cross-bedding and curved marks that reveal flow direction.

  • Conglomerate Types49:25

    Explore conglomerate types, including auto-conglomerates with glass in contact, open vs closed framework, and matrix vs glass-supported structures; assess transport distance, competence, and deduced transport mechanisms.

  • Clastic Rocks Classification58:51

    Learn how clastic rocks are classified by textural maturity, including sorting, roundness, and matrix, with compositional maturity, mineral stability, provenance and tectonic settings, and turbidites.

  • Diagenesis, Lithification & Cements1:01:02

    Explore diagenesis, lithification, and cementation, detailing burial processes—compaction, differential compaction, dissolution, precipitation, and replacement—and how cements shape porosity and permeability.

  • Deep Marine Environment1:11:00

    Explore shallow marine environments, carbonate production, reef types, and ramp forms on the continental shelf. Examine deep marine sedimentation driven by turbidity currents, debris flows, submarine canyons, and accommodation space.

  • Porosity and Permeability1:17:09

    Explore porosity and permeability in sedimentary rocks, covering primary and secondary porosity, granular and micro porosity, and dissolution or fracture porosity, plus total and effective porosity concepts.

  • Buoma Sequence59:59

    Describe the Bouma sequence formed by turbidity currents on steep submarine slopes, showing coarser bottom to finer top sediments and related features like ripple laminations and flame structures.

  • Classification Of Stylolites.1:02:17

    Explore the classification of stylolites by bedding relation and geometry, detailing horizontal, inclined, vertical, cross-cutting and interconnected types, microsatellites, wispy and solution seams, amplitude, contact features, and sedimentary environments.

  • Basin Analysis1:32:21

    Analyze sedimentary basins through subduction geometry, margins, and arc settings, including back-arc and forearc scenarios. Integrate stratigraphy, subsidence, thermal history, and geophysical data to interpret basin evolution.

  • Reynolds, Froude number & Grain Size Scales42:51

    Understand Reynolds and Froude numbers, geometric and logarithmic grain size scales, and viscosity relations to distinguish laminar, transitional, and turbulent flow and associated sedimentary structures.

  • Sphericity Numericals.55:51

    Learn to compute sediment particle sphericity and roundness using six times the particle volume over the sphere diameter, with cylinder, cube, and hemisphere numerical examples.

  • Lagoons, Sedimentary Textures1:17:02

    Explore lagoons as transitional coastal environments, their formation, types (coastal and atoll lagoons), and how sedimentary textures—grain size, sorting, and shape—reveal transgression, regression, and depositional history.

  • Transitional Sedimentary Environments.1:05:36

    Explore transitional marine environments and deltas, including river-dominated bird-foot deltas, tidal-dominated deltas, and Gilbert-type deltas, along with sediment supply, river-mouth morphology, and tidal processes.

  • Dolomitisation and Terms related to Carbonate Classification.1:20:27

    Explore dolomitisation processes, replacement and crystallization in carbonates, and compare mixing-zone, reflex, burial, and seawater models for dolomite formation.

  • Sanstone Questions & Clastic Rock Classification54:24

    Explore sandstone classification using ternary quartz–feldspar–lithic diagrams, assess matrix content, sorting, and textural maturity to identify clastic rock types.

  • Sedimentary Environments.1:01:50

    Learn how sedimentary environments—from continental to deep marine—are controlled by sediment sources, transport processes, and accommodation space, with emphasis on shallow marine dynamics and storm-related structures.

  • Secondary Sedimentary Structures32:25

    Explore secondary chemical sedimentary structures, including concretions and skylights, formed by pressure solution and groundwater-driven mineral precipitation in limestones, with geometric classifications and porosity controls.

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 art

  • Architectural 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 buttresses

  • Ceramics 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 deposits

  • Energy: 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).

Who this course is for:

  • All the Geology Students and those preparing for College, University and other Competitive exams.
  • UPSC, State PSC's and various other exams.