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How to use felsic in a sentence

Looking for sentences and phrases with the word felsic? Here are some examples.

Sentence Examples
In the cooler middle and upper crust, felsic magmatism and aqueous metasomatism are most important.
The alternating bands of mafic and felsic minerals are a striking and distinctive feature of all gneisses.
The occurrence of these felsic extrusive igneous rocks potentially provides key information on the complex interplay of magmatism and tectonics.
Some andesitic and felsic intrusions created a minor, stratified volcaniclastic component via hydrovolcanic eruptions.
It comprises several mafic, mafic-felsic and felsic intrusions with distinctive geochemical affinities and apparent radiometric ages.
Increasing proximity to a subduction zone during plate convergence is indicated by the appearance of felsic tuff.
The rocks of the complex show an overall trend of decreasing mafic minerals and increasing felsic minerals spatially from west to east.
The sample of Omonville granodiorite was collected from the foliated felsic phase of the intrusion at Pointe Jardeheu.
The matrix is dominantly felsic, but also contains biotite, muscovite, epidote and titanite.
These felsic rocks are contemporaneous with or only slightly younger than rocks from the Guevgueli ophiolite.
Their lower viscosity and greater lateral mobility explain why the mafic magmas were distributed over a much wider area than the felsic magmas.
The volcanics are predominantly felsic pyroclastics with lesser intermediate and mafic flows and subvolcanic gabbroic sills and dykes.
The mafic sheets have not contributed at all to the felsic volcanic-derived volcaniclastic breccias, thus supporting an intrusive origin for the mafic volcanic rocks.
It is also possible that upper mantle mafic plumes acted as a heat source for, and made some contribution to, the melting of more felsic rocks in the lower crust.
Also, those workers noted that eclogites, in particular with felsic composition, are theologically weak, relative to their granulitic equivalents.
Voluminous quantities of Late Ordovician to Wenlockian felsic pyroclastics and lava flows record the extensive volcanism associated with the collision and deformation.
The second sector is in the north-west section where the bedrock source likely corresponds to a deformation zone bordering on a felsic intrusion.
In contrast, mafic and felsic intrusive rocks in the Coal Creek inlier are rare.
The horizon is situated north of an intermediate lobate and spherulitic flow and a felsic breccia.
Epiclastic rocks and interbedded fine-grained felsic pyroclastic rocks are dominantly found within the stratigraphic footwall.
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