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    Arrange the following metamorphic facies in increasing order of pressure: (A) Greenschist (B) Eclogite (C) Albite-Epidote hornfels (D) Blueschist C
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    Arrange the following metamorphic facies in increasing order of pressure: (A) Greenschist (B) Eclogite (C) Albite-Epidote hornfels (D) Blueschist
    Choose the correct answer from the options given below:

    A.

    B, A, C, D

    B.

    A, B, C, D

    C.

    A, C, D, B

    D.

    C, A, D, B

    Correct option is D


    The correct answer is (d) C, A, D, B. The increasing order of pressure for the listed metamorphic facies is:
    1. (C) Albite-Epidote hornfels:
    · Forms at low pressure and low to moderate temperature conditions, typically in contact metamorphism settings.
    2. (A) Greenschist:
    · Forms under low to moderate pressure and low temperature conditions, characteristic of regional metamorphism.
    3. (D) Blueschist:
    · Forms under high pressure and low temperature, typically in subduction zones.
    4. (B) Eclogite:
    · Forms under very high pressure and high temperature, characteristic of deep subduction zones.
    Information Booster 1. Albite-Epidote Hornfels Facies:
    · Formed by contact metamorphism with low pressure and moderate temperatures (200°C to 450°C).
    2. Greenschist Facies:
    · Forms at pressures of 2–10 kbar and temperatures of 300°C to 450°C. Minerals include chlorite, epidote, and actinolite.
    3. Blueschist Facies:
    · Forms in subduction zones at pressures of 7–20 kbar and temperatures of 200°C to 500°C. Characteristic minerals are glaucophane and lawsonite.
    4. Eclogite Facies:
    · Forms at very high pressures (greater than 15 kbar) and temperatures of 400°C to 800°C. Characteristic minerals are omphacite and garnet.
    Additional Knowledge · Metamorphic Facies:
    · Distinct sets of minerals that form under specific pressure and temperature conditions.
    · Pressure-Temperature Conditions:
    · Contact Metamorphism: Low pressure, high temperature.
    · Regional Metamorphism: Varies from low to high pressure and temperature.
    · Subduction Metamorphism: High pressure, low temperature.

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