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In general, the margins of continents and areas of mountain constructing are the regions exactly where metamorphic processes continue with intensity. But in reasonably tranquil sites, where sediments accumulate at gradual rates, much less breathtaking alterations also arise in response to alterations in strain and temperature problems. Metamorphic rocks are https://rock-sticks89011.dailyhitblog.com/41753064/everything-about-sticks-of-rock

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