North China
is one of the areas of strong earthquake activity on the Chinese mainland.
Between the 1960s and 1970s, North China experienced the 1966 Xingtai Ms7.2,
1969 Bohai Ms7.4, 1975 Haicheng Ms7.3 and 1976 Tangshan Ms7.8 earthquakes,
causing great losses of life and property. The Tangshan earthquake caused
240,000 casualties. In the past 50 years, Chinese seismologists have conducted
large-scale deep geophysical exploration and research, obtained the detailed
crustal and upper mantle structure, and revealed the deep tectonic environment
of strong earthquakes in North China.
The
resulting research paper has been published in SCIENCE CHINA Earth Sciences by
Professor Wang Chunyong at the Institute of Geophysics, China Earthquake
Administration. The research group reviewed the main achievements of the
studies on the crustal and upper mantle structure as well as the seismogenic
environment and tectonic patterns in North China since the 1966 Xingtai
earthquake.
Based on
plate tectonics theory, geoscientists have successfully explained the patterns
and mechanisms of earthquake activity on global plate boundaries. However,
plate tectonics theory has not explained the occurrence of earthquakes within
the continental plate. The geological structure, seismicity and focal mechanism
of North China's position on the Asian continent show that the seismic activity
is very different from that in the region of the plate boundary, indicating
that the seismotectonics in North China are quite complex. The nucleation,
occurence and development of continental earthquakes, and their relationship
with the deep-seated structure of the Earth are among the most important
subjects in solid Earth science.
Seismologists
have conducted numerous surveys of the crustal and upper mantle structure, and
associated studies of seismic tomography in North China. They have finished 42
deep seismic sounding profiles with total depth of ~12000 km, and seismic
tomography of three-dimensional crustal and upper mantle structure based on the
seismic records at ~600 stations. Deep seismic reflection profiling results
indicate a complex tectonic setting in the strong earthquake areas of North
China, where a listric normal fault and a low-angle detachment in the upper
crust coexist with a high-angle deep fault passing through the lower crust to
the Moho beneath the hypocenter.
Seismic
tomography images revealed that the lithospheric structure in North China is
highly inhomogeneous—most of the large earthquakes occurred in the transition
between the high- and low-velocity zones, and the Tangshan earthquake area is
characterized by a low-velocity anomaly in the middle-lower crust.
Comprehensive analysis of geophysical data demonstrated that the deep
seismogenic environment in the North China extensional tectonic region is
generally characterized by a low-velocity anomalous belt beneath the
hypocenter, inconsistency of the deep and shallow structures in the crust, a
steep crustal-scale fault, relative lower velocities in the uppermost mantle, and
local Moho uplift.
Earthquake
prediction is one of the scientific problems that has not yet been solved.
Thorough understanding of the deep tectonic environment of strong earthquakes
will help to solve the problem of earthquake prediction. Seismologists Deng
Qidong (2008) showed that the surface and shallow-deep tectonic features in the
large earthquake area have been relieved by the combination of deep seismic
reflection profiling and the surface geology and tectonic environment. Thus,
researchers are able to obtain more comprehensive understanding of seismogenic
tectonic conditions in the active fold area (the extension zone and the
compression zone) of the normal or strike-slip normal fault and the reverse
fault.
Despite new
knowledge from deep seismic exploration and seismic tomography, the complexity
of continental seismotectonics still presents some deep-seated problems that
need further research.
Read more
at:
https://phys.org/news/2017-05-deep-seated-tectonic-genesis-large-earthquakes.html#jCp
http://engine.scichina.com/publisher/scp/journal/SCES/60/5/10.1007/s11430-016-9009-1?slug=full%20text
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