Field evidence for active normal faulting in Tibet View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1981-12

AUTHORS

P. Tapponnier, J. L. Mercier, R. Armijo, Han Tonglin, Zhou Ji

ABSTRACT

Crustal thickening does not now occur in southern Tibet. Field observations made during the Chinese–French expedition of 1980 support an earlier hypothesis based on a combined analysis of satellite images and fault plane solutions of earthquakes. Immediately north of the highest peaks of the Himalayas, the tectonic regime is dominated by east–west extension. We have mapped a large number of north–south normal faults which sharply cut the glacial and post-glacial morphology, and followed several recent earthquake breaks along faults detected on satellite and aerial photographs. Microtectonic measurements in the Quaternary suggest that the maximum principal stress is vertical. More... »

PAGES

410-414

References to SciGraph publications

Journal

TITLE

Nature

ISSUE

5840

VOLUME

294

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/294410a0

DOI

http://dx.doi.org/10.1038/294410a0

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1047193584


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