1887

Abstract

Summary

In order, to unravel deformation history of the overturned strata a systematic procedure has been followed: Unfolding strata back to normal position and restoring them using a 2D geomechanics software. Faults formerly considered as strike-slips and thrust faults contemporaneous to Miocene Borneo orogeny here they would be interpreted as syn-sedimentary gravity-driven deformations which suggests an Oligocene-Miocene in age and contemporaneous to West Crocker Formation sedimentation.

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/content/papers/10.3997/2214-4609.201803221
2018-12-03
2020-09-24
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References

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