Kathleen E. Kennedy, Illuminating Media: Transmitting the Renaissance in England, 1400–1550 – Concordia University Press, Spring 2026

Posted on November 17, 2025 by Rashid Faridi

Kathleen E. Kennedy, Illuminating Media: Transmitting the Renaissance in England, 1400–1550 – Concordia University Press, Spring 2026 The overlooked …

Kathleen E. Kennedy, Illuminating Media: Transmitting the Renaissance in England, 1400–1550 – Concordia University Press, Spring 2026
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Afro-Palestinians of Jeursalem

Posted on November 17, 2025 by Rashid Faridi

“They are never spoken about when Palestine is mentioned. Yet they are among the pioneers of the struggle against the Israeli occupation. Here is the…

Afro-Palestinians of Jeursalem
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Petroleum-Bearing Geologic Formations

Posted on November 15, 2025 by Rashid Faridi

Petroleum accumulates in specific geological settings where the right combination of source rock, reservoir rock, caprock, and structural or stratigraphic traps are present. The most likely geology for petroleum bearing includes sedimentary basins with particular rock types and structures.

Key Petroleum-Bearing Geologies

  • Source Rocks: These are usually organic-rich shales or limestones formed from ancient sediments deposited in environments with abundant organic material, such as lakes or marine basins. Over millions of years and under heat and pressure, this organic matter transforms into hydrocarbons.​
  • Reservoir Rocks: The most common reservoir rocks are porous and permeable sandstones and carbonates (limestones, dolomites). These rocks allow for the storage and migration of petroleum. Reservoir rocks must have sufficient porosity (space to hold oil) and permeability (pathways for fluids to move).​
  • Caprocks: Impermeable rocks, like shale or evaporites, act as a seal above reservoir rocks, preventing hydrocarbons from escaping to the surface.​
  • Traps: Petroleum accumulates in traps formed by either structural deformation (folds, faults, salt domes) or changes in rock type (stratigraphic traps, such as buried river channels or reefs). Examples include anticlines, fault traps, and salt dome traps.​

Examples of Petroleum Geology

  • Classic petroleum provinces, such as the Gulf of Suez, contain reservoirs in Cretaceous sandstones and carbonates.​
  • North Sea oil fields have Jurassic sandstones, Triassic alluvial plain deposits, Paleogene deep-sea fans, and chalk reservoirs.​
  • Sandstone, often with secondary silica overgrowth or dolomitization, is the most common reservoir especially in regions like India.​
  • Petroleum fields may also occur in fractured carbonates, reef limestones, and chalks.

Typical Sequence for Oil Fields

Geological FeatureRole in Petroleum SystemExample Rock Type
Source RockGenerates hydrocarbonsShale, organic-rich limestone ​
Reservoir RockStores hydrocarbonsSandstone, limestone, dolomite ​
CaprockSeals reservoir, prevents escapeShale, evaporite ​
TrapHolds hydrocarbons in place for extractionAnticline, fault, salt dome ​
Anticlinal Trap

Fault Trap

Sedimentary basins with organic-rich source rocks, porous and permeable reservoir rocks, effective caprocks, and robust trapping mechanisms are the ideal geological settings for petroleum accumulation and extraction.​

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The Principle of Uniformitarianism : A Fundamental Principle of Geomorphology

Posted on November 13, 2025 by Rashid Faridi

The principle of uniformitarianism in geology is the concept that the natural laws and processes operating today have always operated in the same way in the past, and these processes are sufficient to explain all geological changes observed in Earth’s history. It emphasizes that the present is the key to the past, meaning that by understanding current geological processes, one can interpret past geological events and formations. This principle was first proposed by James Hutton in the late 18th century and later popularized by Charles Lyell.

Uniformitarianism involves several key ideas:

  • Natural laws are constant across time and space.
  • Geological processes observed now operated similarly in the past.
  • Changes typically occur gradually and steadily, although modern interpretations recognize that rates and intensities can vary and that sudden catastrophic events also play a role.
  • The Earth’s geological surface evolves in cycles of erosion, sedimentation, and uplift.

The doctrine serves as a foundation for modern geology by allowing scientists to use present-day observations to infer past geological conditions, rejecting supernatural or catastrophic explanations dominant before its introduction.

Uniformitarianism propounds that the Earth’s features are shaped by continuous and consistent processes over immense periods, making the present the key to understanding the geological past.

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