Question:

The most commonly available minerals in the oceanic crust are:

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Oceanic crust = mafic minerals → olivine + pyroxenes dominate.
Updated On: Jun 12, 2025
  • clinopyroxene, orthopyroxene, olivine
  • quartz, feldspar, mica
  • clinopyroxene, quartz, feldspar, mica
  • orthopyroxene, feldspar, mica
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The Correct Option is A

Solution and Explanation

To determine the most common minerals in the oceanic crust, we need to understand its composition and how it differs from continental crust.

1. Composition of Oceanic Crust:
Oceanic crust is primarily composed of mafic rocks (rich in magnesium and iron) that form from rapidly cooling magma at mid-ocean ridges. The most abundant minerals are:

  • Clinopyroxene (calcium-rich pyroxene)
  • Orthopyroxene (magnesium-rich pyroxene)
  • Olivine (magnesium-iron silicate)

2. Key Differences from Continental Crust:
Unlike continental crust which contains felsic minerals like quartz and feldspar, oceanic crust is dominated by:

  • Basalt (extrusive) and gabbro (intrusive) as primary rock types
  • Higher density minerals rich in Fe and Mg
  • No significant quartz content

3. Mineral Formation Process:
These minerals crystallize from mantle-derived magma in this order:
1. Olivine first
2. Pyroxenes (both clino- and ortho- varieties)
3. Calcium-rich plagioclase feldspar (though less abundant than in continental crust)

4. Scientific Evidence:
Studies of:
- Ophiolite sequences (exposed oceanic crust)
- Deep sea drilling samples
- Mid-ocean ridge basalt (MORB) analysis
all confirm this mineralogical composition

Final Answer:
The most common minerals in oceanic crust are $\boxed{\text{clinopyroxene, orthopyroxene, olivine}}$.

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