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:
2. Key Differences from Continental Crust:
Unlike continental crust which contains felsic minerals like quartz and feldspar, oceanic crust is dominated by:
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 $\boxed{\text{clinopyroxene, orthopyroxene, olivine}}$.