A Cautionary Tale: examples of the mis-location of small earthquakes beneath the Tibetan plateau by routine approaches

Author:

Craig Timothy J1ORCID,Jackson James2,Priestley Keith2,Ekström Göran3ORCID

Affiliation:

1. COMET, School of Earth and Environment, The University of Leeds , Leeds LS29JT, UK

2. Department of Earth Sciences, University of Cambridge , Cambridge CB30EZ, UK

3. Lamont-Doherty Earth Observatory of Columbia University , 61 Route 9W, Palisades, NY 10964, USA

Abstract

SUMMARYEarthquake moment tensors and centroid locations in the catalogue of the Global CMT (gCMT) project, formerly the Harvard CMT project, have become an essential resource for studying active global tectonics, used by many solid-Earth researchers. The catalogue’s quality, long duration (1976–present), ease of access and global coverage of earthquakes larger than about Mw 5.5 have transformed our ability to study regional patterns of earthquake locations and focal mechanisms. It also allows researchers to easily identify earthquakes with anomalous mechanisms and depths that stand out from the global or regional patterns, some of which require us to look more closely at accepted interpretations of geodynamics, tectonics or rheology. But, as in all catalogues that are, to some extent and necessarily, produced in a semi-routine fashion, the catalogue may contain anomalies that are in fact errors. Thus, before re-assessing geodynamic, tectonic or rheological understanding on the basis of anomalous earthquake locations or mechanisms in the gCMT catalogue, it is first prudent to check those anomalies are real. The purpose of this paper is to illustrate that necessity in the eastern Himalayas and SE Tibet, where two earthquakes that would otherwise require a radical revision of current geodynamic understanding are shown, in fact, to have gCMT depths (and, in one case, also focal mechanism) that are incorrect.

Funder

Natural Environment Research Council

Royal Society

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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