LITHOSTRATIGRAPHY

Learn about lithostratigraphy, the study of rock layers, and its importance in understanding Earth's geological past. Explore the principles and applications of this vital field.

Apr 11, 2022 - 02:00
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LITHOSTRATIGRAPHY
  1. Lithostratigraphy
  • Lithostratigraphy is a scientific practice that examines the physical and mineralogical properties of rock layers, often known as strata.
  • This subject pertains to the categorisation and association of rock units.
  • Objective: To analyse the arrangement, makeup, and chronological order of rock formations, therefore facilitating the reconstruction of previous geological settings and better comprehension of the geological history of a certain region.

 

  1. Fundamental Principles
  • Lithologic units refer to rock strata that are characterised by their specific physical and mineralogical features.
  • Facies refer to unique rock features that indicate the circumstances under which rocks were formed and may be used to deduce previous environments.
  • Correlation refers to the procedure of establishing an association between rock strata from various geographical areas by analysing their lithological characteristics.

 

  1. Units Based on Lithostratigraphy

Literature Description

  • Texture: particle size (e.g., sediment, granulated rock).
  • Composition: found mineral and rock kinds.
  • Colouration: Effects of mineral composition and weathering.

 

There exist several categories of lithostratigraphic units:

  • Formation in lithostratigraphy refers to a basic unit that is identifiable and can be mapped, characterised by consistent lithologic features.
  • A member refers to a subdivision of a formation, which is a smaller and unique layer or group of layers within that formation.
  • Bed: the most basic lithostratigraphic unit; a single layer exhibiting consistent properties.
  • A group refers to a set of two or more formations that have similar lithological features and are grouped together for the purpose of statistical correlation.

 

4. Identification of Lithostratigraphic Classification

1. Lexical Classification

  • Clastic rocks are deposits of sediment particles such as sandstone and shale.
  • Chemical rocks are formed by precipitation from a solution, such as limestone or evaporites.
  • Igneous rocks are formed from geologically solidified magma, such as basalt or granite.

 

2. Investigation of Facies

  • Depositional Environment: Analysing facies to recreate historical ecosystems like rivers, lakes, or marine habitats.
  • Facies change refers to the study of transitions between distinct facies in order to gain insight into geological history and processes.

 

5. Lithostratigraphic Correlation

Main ideas

  • The principle of lithologic continuity states that units with comparable lithological properties may be tracked over vast regions.
  • Principle of Superposition: In undisturbed sequences, the older layers are positioned under the younger layers.
  • Principle of Lateral Continuity: Layers initially expand horizontally in all directions until they become thinner or come into contact with a physical obstruction.
  • Methods: Field Mapping: The act of seeing and recording rock units and their interrelated structures in the field.
  • Geophysical surveys include techniques such as seismic reflection to cartograph subsurface rock units.
  • The process of drilling and core sampling involves the extraction of rock samples from the subsurface in order to examine lithological characteristics.

 

 6. Case Studies

  • Sedimentary basins: analysing sedimentary strata within basins to get insights into the geological history of local areas.
  • Analysis of volcanic deposits in volcanic regions to track volcanic activity and its effects on the adjacent rock strata.
  • Tectonic settings refer to the study of rock units in regions of tectonic activity in order to get valuable insights on deformation and structural geology.

 

7. Practical Uses

  • Resource exploration is the identification and mapping of rock units in order to find and extract natural resources such as oil, gas, coal, and minerals.
  • The assessment of rock units in environmental studies is conducted to get insights into groundwater movement, pollution, and land use planning.
  • Geological mapping involves the creation of comprehensive geological maps for academic, engineering, and planning objectives.

 

IMAGE SOURCE (THUMBNAIL)

 

 

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arulprasanth Arul Prasanth - MSc Geology graduate offering comprehensive study materials in Geology, Physics, and English. With a focus on clarity and effectiveness, I aim to provide students with the tools necessary for academic success.