Part-4: Clastic Depositional Environment -Empower Your Geoscience Journey: Top Free Public Resources for Geological Learning

Part-4: Clastic Depositional Environment -Empower Your Geoscience Journey: Top Free Public Resources for Geological Learning

Depositional environment is a very interesting topic which involves geological analytical thinking to solve a problem. In this part i am sharing very key fundamental details & its resources which are critical for clastic depositional Environments.

A depositional environment simply refers to the specific type of place where sediments accumulate and become sedimentary rocks/formation. These environments vary greatly and are influenced by factors such as climate, tectonic activity, and the type of material being deposited. They play a crucial role in determining the characteristics of the resulting sedimentary rocks.

1. Significance of Depositional Environments

  • Interpretation of Past Environments: By studying sedimentary rocks and their characteristics, geologists can infer the conditions of ancient depositional environments.
  • Resource Exploration: Understanding depositional environments helps in locating natural resources such as coal, oil, natural gas, and certain types of minerals.
  • Environmental Reconstruction: Provides insights into past climate changes, sea level fluctuations, and tectonic movements.
  • Petroleum system elements : Depositional environments are crucial for hydrocarbon exploration for several reasons, primarily because the formation, migration, and accumulation of hydrocarbons (oil and natural gas) are directly influenced by the characteristics of these environments, This knowledge is used to build geological models and guide exploration drilling.
  • Reservoir Quality: Depositional environments influence the texture, grain size, sorting, and mineral composition of reservoir rocks, affecting their quality. Understanding these properties helps in evaluating potential reservoirs.
  • Reducing Exploration Risk: Detailed knowledge of depositional environments reduces the risks associated with exploration

There are several resources availble on Clastic Depositional environment, here i am highlighting few very concise references which are available free in public. However several case studies and published books can be referred for more clarity on this subject.

Brief Descriptions of sedimentary Environments can be obtained from the below resources,

2. Categories of Depositional Environments

Depositional environments are divided into three main categories: terrestrial (on land), transitional (at the margins between land and ocean), and marine. Below table lists the depositional environments in these settings organized according to whether they are in clastic- or carbonate-dominated systems.

3. Factors Influencing Depositional Environments

Several Factors which influence clastic depositional systems asre shown in the below diagram,

Factors which influence clastic depositional systems. Richards et al. (1998). Reprinted with permission of Geol. Soc. London.

4. 3D Block diagrams of Depositional Environments

Several 3D Block diagrams represening differnt sedimentary environments are provided as follows for better understanding can be found below

Some of the important depositional environments for sediments and sedimentary rocks. Source: Karla Panchuk (2021) CC BY-SA 4.0. Modified after Mike Norton (2018) CC BY-SA 3.0
A representation of common depositional environments
An idealised panorama of depositional systems across a range of terrestrial and marine environments.
A schematic model display the different depositional environment and the the interpreted tidal environment (adapted from Sa?ag et al. 2016)

5. Key Characteristics of Depositional Environments

The table below includes specific environments where various types of sediments are deposited and common rocks, structures, and fossils that aid in deducing the depositional environment from examining a sedimentary rock outcrop.

Depositional Environments Table

Below Simplified tables shows what to look for in the rock record in specific Depositional Environment.

Key characteristics of specific Depositional Environment
Properties can be used to interprete depositional environment

From different sources Similar tables provides a summary of the processes and sediment types, associated rocks that pertain to the various depositional environments .

Terrestrial Depositional Environments.
Marine & Transitional Depositional Environments
Continental Sedimentary Environments
Transitional Sedimentary Environments
Marine Sedimentary Environments
Depositional Environments & associated elements
Common depositional environments and their corresponding sedimentary rocks
Typical colors of sedimentary rocks based on their depositional environment and oxygen availability during burial and lithification. Image credit: Daniel Hauptvogel, CC BY-NC-SA
Grain characteristics used to infer the relative distance that sediments have travelled from their source rock. a) Sorting of sediment; b) Sediment roundness, often called sphericity. Image credit: a) Adapted from Wikimedia user
Compositional and Textural Maturity helps to interpret Common Environments

6. Analog Examples of Depositional Environments

Below table provides several depositional environments and their analogue examples

Summary of different depositional environments, stratigraphic characteristics and facies model with modern, ancient and oil field examples

Find below an Excellent read on Shallow-marine Sandstone Reservoirs, Depositional Environments, Stratigraphic Characteristics and Facies Model: A Review

https://scialert.net/fulltext/?doi=jas.2017.212.237

7. Role of Depositional Environment in Hydrocarbon Exploration

Environments where bioproductivity and depositional environment favour the accumulation of organic-rich sediments.

Depositional environments favouring the accumulation of petroleum source rocks are illustrated in above figure in the context of a section through a tectonic plate. The amount of kerogen present in sediments is a balance between bioproductivity, survival, and dilution by inorganic grains. we can consider some extremes as below:

  1. Low productivity—Aeolian (wind-blown) desert sandstones where land plant growth is restricted due to the extremely arid environment.
  2. High productivity—Areas of ocean upwelling where the enhanced supply of nutrients fuels explosive growth of phyto- and zooplankton.
  3. Poor survival—Chalk composed almost exclusively of coccolith skeletal debris (high bioproductivity) but where all the coccolith body tissues are destroyed by bacterial activity under strongly oxic open marine conditions.
  4. Excellent survival—Early rifting phases of oceans where both optimum sedimentation rates and anoxic conditions of the lakes and enclosed seaways promote high rates of organic matter preservation.
  5. Strong dilution—The prolific sediment supply of major deltas produces organic lean delta-front and pro-delta sediments despite high bioproductivity.
  6. Minimal dilution—Coals where the lignocellulosic and other tissues of high-productivity land plants are well preserved in a delta-top environment starved of (or bypassed by) mineral grains.

Thus to summarize the optimum oil-prone source rocks are deposited where anoxia develops in an aqueous environment enjoying high rates of sedimentation. The combination of high sedimentation rates and oxic environments favours the accumulation of gas-prone source rocks such as coals.

Summary of major processes controlling petroleum source rock accumulation (red?=?gas-prone; green?=?oil-prone).

8. Types of data used to determine the Depositional Environment

Types of data commonly used in facies analysis/depositional environment of clastic rocks

One of the initial steps in depositional environment analysis is facies analysis. This involves the description and interpretation of conventional core samples from a clastic reservoir. Core description allows for the subdivision of these cores into lithofacies, which are defined by characteristics such as lithology, grain size, physical and biogenic sedimentary structures, and stratification, all of which relate directly to the depositional processes that created them. Lithofacies and lithofacies associations (groups of related lithofacies) serve as the fundamental units for interpreting depositional environments, Example provided as below,

Sedimentary processes, lithofacies, and lithofacies associations for a meandering channel sequence. (The vertical sequence is modified from Walker

Below is a simplistic 3D depositional environment model with basic log response for reference,

Models of major depositional environments. The curve on the left shows the SP or gamma ray response and the curve on the right shows the relative grain size profile. The size of the dots next to the vertical profile indicates the relative magnitude of permeability expected in such a sequence. (Parts c and d are from Walker, 1984, and parts f, h, and i are from Galloway and Hobday, 1983.)

9. Quick Exercises to test your knowledge

Below are few key resources with examples and exercises to test your knowledge and improve understanding.

References

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Disclaimer: The views expressed in this article are solely those of the author and do not necessarily reflect the official policy or position of any organization, institution, or individual mentioned within the text. The author acknowledges that opinions, interpretations, and information presented may be subject to errors, omissions, or inaccuracies. The author takes no responsibility for any consequences arising from the use of information contained in this article. Readers are encouraged to independently verify and cross-reference all information before making any decisions or taking any actions based on the content of this article. Please contact author to remove any copyright elements.




Madhuwanti Sahoo

Geoscientist at Schlumberger Asia Services Limited,Mumbai

5 个月

Thank you sir for such helpful and informative shares.

Soumya Prakash Tripathy

Senior Geologist @ Oilmax Energy | Static Reservoir Modeling, CCS, Natural Hydrogen

5 个月

Thank you sir for sharing.?? This is extremely useful and informative.

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