| Institute of Geomechanics, Chinese Academy of Geological Sciences | Host |
| Citation: |
LAO Xiong. 2000. ON THE FORMATION OF THE BANGONG-CO-NUJIANG FAULT ZONE. Journal of Geomechanics, 6(1): 69-76.
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ON THE FORMATION OF THE BANGONG-CO-NUJIANG FAULT ZONE
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Abstract
The Bangong-Co-Nujiang fault zone consists of four arcuate faults.The zone was subsided successively from north to south to receive sediments derived from the two immediately adjoining uplifted flanks in the late Triassic to the Cretaceous.It was the results of undulated earth's movement. -
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LAO Xiong. 2000. ON THE FORMATION OF THE BANGONG-CO-NUJIANG FAULT ZONE. Journal of Geomechanics, 6(1): 69-76.
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