Show diagrammatically the characteristics of binary eutectic system under 1 atmosphere (1 atm pressure). How does one explain the formation of porphyritic basic rock with phenocryst of plagioclase in a groundmass with plagioclase and clinopyroxene with the help of a suitable binary eutectic system? IAS 2024, 10 Marks

Show diagrammatically the characteristics of binary eutectic system under 1 atmosphere (1 atm pressure). How does one explain the formation of porphyritic basic rock with phenocryst of plagioclase in a groundmass with plagioclase and clinopyroxene with the help of a suitable binary eutectic system? IAS 2024, 10 Marks

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Introduction:

  • A binary eutectic system consists of two components that form a eutectic mixture at a specific composition and temperature.
  • The characteristics of a binary eutectic system under 1 atm pressure can be represented diagrammatically.

Characteristics of Binary Eutectic System Under 1 Atmosphere

Key Features:

  • A binary eutectic system involves two components that can coexist as liquid and solid at a specific eutectic composition and temperature under 1 atm pressure.
  • Phases: Includes liquid, solid A, and solid B.
  • Eutectic Point: The lowest temperature at which the liquid phase can exist; both components crystallize simultaneously in a fixed ratio.

Diagram Explanation:

  • The phase diagram consists of:
    • Liquidus Curve: Separates the liquid phase from the two-phase liquid + solid region.
    • Solidus Curve: Indicates temperatures below which only solid phases exist.
    • Eutectic Point: Intersection of solidus and liquidus lines where the two solids crystallize simultaneously.

Simplified Diagram:

Formation of Porphyritic Basic Rock with Plagioclase Phenocrysts

Explanation with Binary Eutectic System:

  • System: Consider the diopside-anorthite system as a representative binary eutectic system.
  • Initial Stage:
    • The magma initially cools slowly at depth, leading to the formation of large plagioclase phenocrysts (early crystallization due to supercooling).
    • Plagioclase forms due to the liquidus curve's inclination toward the plagioclase composition.
  • Subsequent Cooling:
    • As the magma cools further, it reaches the eutectic point.
    • Both plagioclase and clinopyroxene crystallize together from the remaining liquid.
  • Final Rock Texture:
    • The phenocrysts of plagioclase (formed earlier) are embedded in a fine-grained groundmass composed of plagioclase and clinopyroxene, reflecting the eutectic crystallization.

Relevance of Binary Eutectic System:

  • The eutectic system explains the simultaneous crystallization of plagioclase and clinopyroxene in the groundmass.
  • The earlier nucleation of plagioclase corresponds to the solidus-liquidus path of a plagioclase-rich composition.

Diagram:

Conclusion:

  • The characteristics of a binary eutectic system under 1 atm pressure can be represented diagrammatically.
  • The formation of porphyritic basic rock with phenocrysts of plagioclase can be explained using a binary eutectic system with plagioclase and clinopyroxene.