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Within this depression another major fault forms the Qoltag Mountains, which divide the basin into two sections.
A major fault forms the eastern limit of the deposit, beyond which, Archaean basement rocks (Pre-Cambrian) are present immediately below the Dupi Tila.
At this site, the fault forms a nearly 500-m high scarp (Figure 3a), and the fault tip reaches the surface at the foot of the scarp.
In particular, the multiply reactivated Middle Bore Fault forms a major crustal boundary and is interpreted to mark the northern limit of the Gawler Craton.
The fault forms a steeply dipping contact (based on MT data) of the Paleozoic sedimentary rocks with Cenozoic alluvial fan deposits and the underlying coarse-clastic sediments of the Mae Fang Formation.
Field studies predict that pull-apart basins become extinct when an active basin-crossing fault forms; this is the most likely fate of pull-apart basins, because basin-bounding strike-slip systems tend to straighten and connect as they evolve.
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Researchers suspect the fault formed as huge slabs of earth collapsed into the initial crater.
This is considered to represent a preexisting fault formed before subduction began.
We show the existence of a northward-dipping detachment fault formed at the beginning of the exhumation phase (Burdigalien).
The North Anatolian fault (NAF) is one of the largest currently active dextral strike-slip fault forming the plate boundary between Eurasia and Anatolia.
Oblique-slip (sinistral normal) fault zones located at the southern termination of the Bolfin fault form a well-developed imbricate fan structure.
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