Question:

Choose the correct combination(s) of textural features of magmatic rocks with corresponding petrological processes from the following.

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Magmatic textures such as ophitic, perthitic, and spinifex are key to understanding the cooling history and crystallization processes of igneous rocks.
Updated On: Nov 18, 2025
  • ophitic texture in dolerite - peritectic crystallization
  • perthite in granite - slow subsolidus cooling
  • spinifex texture in komatiite - eruption of ultramafic lava
  • orthopyroxene rim around olivine in peridotite - eutectic crystallization
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The Correct Option is A

Solution and Explanation

Step 1: Understanding the question.
This question asks about the relationship between magmatic textures and the processes that create them. Textures like ophitic and perthite are linked to specific petrological processes.
Step 2: Analyzing the options.
(A) ophitic texture in dolerite - peritectic crystallization: Correct — Ophitic texture is common in rocks that crystallized through peritectic crystallization.
(B) perthite in granite - slow subsolidus cooling: Correct — Perthite forms during slow cooling, often in granitic rocks, through exsolution.
(C) spinifex texture in komatiite - eruption of ultramafic lava: Correct — Spinifex texture is a characteristic feature of komatiites, which are ultramafic lava flows that cool rapidly.
(D) orthopyroxene rim around olivine in peridotite - eutectic crystallization: Incorrect — This texture is more related to the crystallization sequence in peridotites and is not a result of eutectic crystallization.
Step 3: Conclusion.
The correct answer is (A), (B), (C). These are correct combinations of textures and the petrological processes responsible for their formation.
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