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- W3152171477 abstract "The deep structure of the Tianshan earthquake belt is investigated,based on the seismic tomography of the northwestern China. The result indicates that a ductile detachment layer with low velocities exists in the mid-crust of the Tianshan earthquake belt; the fault in the southern Tianshan extands beyond the depth of the Moho, while the fault in the northern Tianshan only reaches mid-crust; the depth of the Moho of the Tianshan is more than 50km, moreover, the crust-mantle boundary is composed of a wide velocity transition belt. Strong earthquakes are mainly concentrated in the mid-lower crust where a sharp velocity variation is observed near the basin-mountain boundaries. A low velocity zone is found between the Pamir, southern Tianshan and Tarim, with an orientation of NNE. The earthquakes in Wuqia and Jiashi are separately located in the west and east sides of this low velocity zone. It is inferred that the relative inchon of the Pamir, southern Tianshan and Tarim is a major reason to cause deformation occurring within this low velocity zone and fracturing near its boundaries. Besides, the intrusion of hot mantle has played an important dynamic role in tectonic activities in this region." @default.
- W3152171477 created "2021-04-13" @default.
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- W3152171477 date "2000-01-01" @default.
- W3152171477 modified "2023-09-25" @default.
- W3152171477 title "CRUSTAL STRUCTURE AND TECTONIC ENVIRONMENT OF STRONG EARTHQUAKES IN THE TIANSHAN EARTHQUAKE BELT" @default.
- W3152171477 hasPublicationYear "2000" @default.
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