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Plio-Quaternary kinematic development and paleostress pattern of the Edremit Basin, western Turkey
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文摘

Edremit Basin has been opened due to the right stepover of two right lateral fault zones.

The Edremit Basin has typical geometry of transtensional pull-apart.

We perform fault-slip inversion of heterogeneous fault populations.

Two superposed local stress fields are detected.

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