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Parasequence

Concept of sequence stratigraphy From Wikipedia, the free encyclopedia

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A parasequence is a fundamental concept of sequence stratigraphy. Parasequences are not directly related to sequences.

Definition

A parasequence is defined as a genetically related succession of bedsets that is bounded by marine flooding surfaces (or their correlative surfaces) on top and at the bottom.[1] The succession is supposed to be relatively conformable in the sense that breaks in deposition within the parasequence are much shorter than the time of deposition of the parasequence itself.[2][1] Most parasequences show a shallowing upward,[3] which is sometimes also included into the definition.[4]

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Schematic graphic log showing facies successions in common types of clastic parasequences
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Schematic graphic log showing facies successions in common types of carbonate parasequences
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Properties

Since parasequences are relatively conformable, so Walther's law applies within a parasequence. This is not necessarily the case for transitions from one parasequence to another. They are also typically of the size of one up to tens of meters.[3]

References

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