Abstract
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 that the basin experienced pull-apart opening with rapid subsidence of the central blocks. Combined with the outcrop data on asymmetric lithofacies distribution, facies transitions, and paleoflow directions of the alluvio-lacustrine systems, the MT data help explain basin-fill processes during basin formation. The high-frequency MT technique is a useful substitute for the costly burden of a seismic-reflection survey.
| Original language | English |
|---|---|
| Pages (from-to) | 101-109 |
| Number of pages | 9 |
| Journal | Sedimentary Geology |
| Volume | 129 |
| Issue number | 1-2 |
| DOIs | |
| State | Published - 1999.11 |
Keywords
- Basin analysis
- Cretaceous
- Korea
- Magnetotellurics
- Pull-apart basin
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