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The Turpan Basin has a complex polycyclic sedimentary and tectonic history from Late Permian to late Tertiary time. Main stratigraphic boundaries are unconformities that bound tectonically induced sedimentary cycles. The depositional style reflects a continental environment exhibiting changes from alluvial fan/fluvial to lacustrine conditions within each cycle. More than 7000 m of clastic sediments...
A new high-resolution magnetotelluric (MT) survey in a pull-apart basin (Cretaceous Eumsung Basin, Korea) provides integrated images of internal architecture. Two cross-basinal MT profiles show an asymmetric form with a subbasin in the southeastern part and these characteristics are reflected well in paleoflow directions and facies transitions of the surface lithofacies units. The results suggest...
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