Characteristics of Faults and Folds by Using Subsurface Structural Data in Dogye Area, Korea

지하(地下) 석탄층(石炭層) 구조(構造)를 이용한 도계(道溪) 지역의 단층과 습곡구조의 특성

Structural interpretation by using subsurface attitude of coal seam and outcrop patterns of folds and faults shows that wrench and thrust tectonics took place simultaneously in the study area. From the interference patterns of fold axes, three generations of folding are suggested: $F_1$ (NE-SW), $F_2$ (N-S), and $F_3$ (E-W). Differential displacement of rock mass from north to south yields to E-W fold and Osypcheon Fault. Geometry of subsurface coal seam show different patterns comparing to those of surface outcrop because of shallow-depth crustal shortening which took place post Cretaceous.