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How to use metamorphism in a sentence

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

Sentence Examples
These are actually pseudomorphs of sericite after cordierite and are found included in hornfels or slate as a product of contact metamorphism.
Early crustal thickening was associated with high-grade metamorphism of the basement and is kinematically complex.
Field relations indicate that intrusion post-dated the peak of regional metamorphism and the main foliation-forming event.
Two phases of regional metamorphism are related to their respective episodes of penetrative deformation in the southern Central Iberian Zone.
From Pliocene time the shallow emplacement of intrusive bodies resulted in thermal metamorphism and hydrothermal activity.
In contrast to parts of the External Hellenides, the Menderes nappes do not show Tertiary high-pressure metamorphism.
Baked contacts with host rocks indicate that metamorphism associated with intrusion predates shearing.
Both thrust and normal faults initiated synchronously with Miocene prograde metamorphism and melting, and have moved episodically since then.
No such difference in the pressure or temperature of metamorphism in the country rock is detectable.
Later, shallower and hotter metamorphism produced widespread sillimanite grade gneisses, migmatites and in situ partial melting.
He regarded metamorphism and deformation as continuously related processes and found it impossible to accept migmatites as metamorphic rocks.
The Dalradian of NE Scotland is a discrete lithotectonic unit and the type locality for Buchan-type high-T, low-P regional metamorphism.
The sequence shows retrogression from blueschist to greenschist facies metamorphism during deformation.
Uvarovite is formed from the metamorphism of impure siliceous limestones and some other rocks that contain chromium.
Vesuvianite forms as a result of contact metamorphism on impure limestones and is usually found with other exotic minerals.
The raw material source is a steatitic talc, also called soapstone, which originates from the thermal metamorphism of siliceous dolomitic rocks.
A very low-grade metamorphism, which developed chloritoid, affects cleaved rocks.
These rocks were later affected by low-grade metamorphism under high geothermal gradients.
It also occurs as a secondary mineral associated with contact metamorphism of limestone.
As there is no sign of contact metamorphism in the limestones, we interpret this to be a normal fault.
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Examples from Classical Literature
Corundum is a product of contact metamorphism and also a result of direct crystallization from molten magma.
Garnets result mainly from contact metamorphism, and commonly occur either in schists and gneisses or in marble.
The birthplace of a large variety of ores and minerals is in the zone of metamorphism.
Sapphire, ruby, emerald, and tourmaline result also from contact metamorphism of sediments in the vicinity of igneous rocks.
In contact metamorphism, thin sheets of molten rock produce less effect than thicker ones.
The subject, however, is a complex one, the full discussion of which belongs in treatises on metamorphism.
Certain kinds of metamorphism are suggestive of the nature of the mineral deposits with which they are associated.
Lapis lazuli usually occurs in crystalline limestone, and seems to be a product of contact metamorphism.
Contact metamorphism along both the quartz-porphyry and the diorite contacts was practically lacking.
Amorphous graphite is formed in many places where coal and other carbonaceous materials have undergone extreme metamorphism.
Hence it is that the subject of contact metamorphism is of interest to economic geologists.
A common cause of the metamorphism of rocks is the intrusion into them of igneous rocks.
All of the chemical, mineralogical, and textural changes in rocks above described may be collectively referred to as metamorphism.
The rock has undergone complete metamorphism and its origin is unknown.
The metamorphism is related not only to overthrusting and the obduction of oceanic crust but also to a subduction zone setting.
Sharygin said that of the many fragments we've been analysing, only three dark samples show strong evidence of earlier metamorphism and melting.
This is called contact metamorphism or thermal metamorphism.
Nor is the metamorphism of the invaded rock limited to simple intrusion.
How is metamorphism on the large scale supposed to have been induced?
The metamorphism is more striking in the first change than in the second.
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