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《Chinese Journal of Geophysics》 1988-04
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SEISMIC REFRACTION AND REFLECTION PROFILINGS ACROSS TANGSHAN EPICENTRAL REGION AND THEIR IMPLICATION TO SEISMOGENIC PROCESSES

ZENG RONG-SHENG LU HAN-XING DING ZHI-FENG(Institute of Geophysics, State Seismological Bureau)  
Seismic refraction and reflection profilings across Tangshan epicentral region have depicted a clear picture of the crustal structure in this area, where a large earthquake of magnitude 7.8 occurred in 1976.A paleozoic syncline of Kaiping, located just east of Tangshan city is a nearly vertical right lateral strike-slip fault, broken throughout the whole crust. This fault has been activated in recent time. Its horizontal displacement with. NNE direction accounts for the horizontal surficial strain during the occurrence of Tangshan earthquake. The western flank of Kaiping syncline is associated with Douhe fault a normal fault striking NNE and dipping southeas-twards to a depth of about 5 km, with a dipping angle of 26°. The Douhe normal fault extends right over the epicentral region of Tangshan City. The vertical surficial strain during the great earthquake is produced by the displacement of this normal fault. The focal depth of both the main shock and the aftershocks are about 5-22 km. The deformation at this depth-range revealed from the reflection profile is different from that in the upper 5 km medium of this region. An analysis of the thermodynamic properties in the deep crustal medium has shown that transition layers consisting of alternating "brittle" and "ductile" material may prevail at the seat of earthquakes.The simultaneous occurrence of the horizontal displacement of the Kaiping Crustal Break and the movement of Douhe normal fault requires that an extensional force should exist in addition to the regional horizontal compression prevailing in North China Plain. The chaotic dipping of reflections in the upper crust and a prominent offset of 3-5 km of Moho discontinuity highly suggest that the migration of hot material from the uppermost mantle to the crust may occur in Kaiping crustal break. The thermal stress of a hot crustal channel can produce an extensional stress in the upper crust and a compressional stress in the lower crust. It explains the seismic reflection profile pretty well. The migration of hot material in Kaiping Crustal Break has two effects on the occurrence of the earthquake: it produces additional extension in the upper crust which activates the motion of Douhe normal fault, and also softens the material in Kaiping crustal break so that his strike slip fault becomes easier for moving.
【Fund】: 地震科学联合基金
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