How to practice topic:metamorphic-petrology

Attempt a question, record the concept and assumptions, then check the available answer. Rework mistakes after revising the relevant concepts. Topic tags can overlap; review the question context.

Questions 1–10 of 29. Imported answers require independent review unless marked reviewed.

Topic practice 29 questionsPage 1 of 3

Question 41

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For a chemical system with 5 phases at the invariant point, the number of possible univariant reactions in pressure-temperature space is _____ (answer in integer).

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Question 45

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Which one of the following mineral reactions will result in the formation of a diagnostic granulite facies assemblage during regional metamorphism of a pelite?
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Question 56

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The given schematic diagram shows different stages of development of S₂ foliation after the formation of S₁ foliation. Which of the following statements CORRECTLY interpret(s) the relationships of porphyroblasts W, X, Y and Z with the matrix?
Diagram for Geology and Geophysics question 56

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Question 63

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The Fe-Mg exchange reaction between olivine and spinel is the following:
Mg₂SiO₄ + 2FeAl₂O₄ ↔ Fe₂SiO₄ + 2MgAl₂O₄ (Fosterite) (Fe-spinel) (Fayalite) (Mg-spinel)
Assuming ideal solid solutions, the temperature of equilibrium between olivine and spinel using the following data is __________ °C (round off to nearest integer).
[Assume that ΔHᵣ⁰ and ΔSᵣ⁰ are independent of P and T, and Kd is independent of P]
| ΔHᵣ⁰ (kJ/mol) | ΔSᵣ⁰ (J/mol. K) | Kd = [(xFe^Ol xMg^Sp)/(xMg^Ol xFe^Sp)]² | R (J/mol. K) | | −10.91 | −3.90 | 3.024 | 8.314 |

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Question 39

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Which of the following rock and texture combinations is/are CORRECT?
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Question 41

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Which of the following rocks is/are characteristic of fossil subduction zones?
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Question 62

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In the isochemical phase diagram shown below, the curved arrow represents the P-T path. The variance at peak metamorphism is __________
Diagram for Geology and Geophysics question 62

(Answer in integer)

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Question 30

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Match the microstructures in Group–I with their characteristics in Group–II.
Group–I: P. Core–mantle; Q. Decussate; R. Spherule; S. Millipede
Group–II: 1. Radiating fibrous aggregate of K-feldspar with or without quartz; 2. Large strained mineral grains surrounded by fine-grained, recrystallized grains; 3. Inclusion trails in a porphyroblast curves into the matrix foliation by developing concave outward pattern; 4. Randomly oriented mineral grains dominated by crystal faces, such as in sheet silicates
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Question 32

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Which one of the following sequences of index minerals correctly represents the order of increasing metamorphic grade during regional metamorphism of siliceous dolitic limestones?
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Question 49

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During high-temperature metamorphism of pelites, which one of the following mineral reactions represents the second sillimanite isograd?
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