If folds like anticlines and synclines form because of compression of the earth’s crust, and reverse and thrust faults form due to compression as well, the reason why some rocks bend and others break during this compression is due to their stress capacity which is derived for the capacity and chemical constituent of the rocks.
<h3>What are
anticlines?</h3>
An anticline is a form of fold in structural geology that has an arch-like structure and its oldest beds near its center, whereas a syncline is the inverse of an anticline.
An anticline is a convex upward fold, whereas a syncline is a concave upward fold. An anticlinorium is a huge anticline with minor folds superimposed on it, whereas a synclinorium is a large syncline with minor folds superimposed on it.
Anticlines provide a structural trap that can trap pockets of hydrocarbons in the arch's bend. In the anticline peak, impermeable rock layers, sometimes known as seals or cap rock, trap hydrocarbons. This allows oil and natural gas to accumulate in the pores of the reservoir rock near the arch's core.
Learn more about synclines:
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