Questions 151–160 of 650. Imported answers require independent review unless marked reviewed.

Topic practice 650 questionsPage 16 of 65

Question 21

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Which of the following Epochs belong(s) to the Quaternary Period?
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Question 22

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Which one or more of the following minerals shows O:Si ratio of 4:1 in its silicate structure?
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Question 23

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Which of the following rock structures is/are fold(s)?
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Question 24

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Assume heat producing elements are uniformly distributed within a 16 km thick layer in the crust in a heat flow province. Given that the surface heat flow and reduced heat flow are 54 mW/m² and 22 mW/m², respectively, the radiogenic heat production in the given crustal layer in µW/m³ is ____________ (in integer).

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Question 25

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A confined aquifer with a uniform saturated thickness of 10 m has hydraulic conductivity of 10⁻² cm/s. Considering a steady flow, the transmissivity of the aquifer in m²/day is _________________ (rounded off to one decimal place).

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Question 26

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A current of 2 A passes through a cylindrical rod with uniform cross-sectional area of 4 m² and resistivity of 100 Ω-m. The magnitude of the electric field (E) measured along the length of the rod in V/m is ______________ (in integer).

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Question 27

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Which one of the following lineations can be observed on a foliation with an attitude 210°, 40° NW?
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Question 28

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Match the minerals in Group–I with the corresponding cleavage types in Group–II.
Group–I: P. Diopside; Q. Galena; R. Calcite; S. Fluorite
Group–II: 1. Cubic; 2. Octahedral; 3. Prismatic; 4. Rhombohedral
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Question 29

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The composition of which one of the following reservoirs closely matches with that of iron meteorites?
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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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