Triangles: 492.9k
Vertices: 250k
More model informationA large exposure of geologically complex structures composed of folds and detachment faults. The succession shows a package of carbonate rock interbedded with thin shale layers and squeezed shale. The rocks are deposited during The Triassic period in carbonate platform environment and the structure is form associate with Indosinian orogeny. The major trends of the fold axis in this area have two directions. The first one is in the NE-SW direction, and the second one is in the E-W direction. Also, the fault planes trend is along the E-W direction.
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