The main study results of depth seismic sounding in the northeastern margin of Qinghai-Tibetan plateau(32°-40°N, 100°-108°E) are reviewed and summirized in this paper. The crustal structure characteristic of seismic wave velocity and the shape of the Moho in this area are given.
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周民都.青藏高原东北缘深地震测深研究成果回顾[J].地震工程学报,2006,28(2):189-191. ZHOU?Min-du. Review of Study on the Depth Seismic Sounding in the Northeastern Margin of Qinghai -Tibetan Plateau[J]. China Earthquake Engineering Journal,2006,28(2):189-191.