横过青藏高原羌塘地体中央隆起区的深反射地震试验剖面

跨越中央隆起区的深反射地震探测试验剖面，初步揭露出青藏高原羌塘地体中央隆起区的地壳结构.探测剖面表明，羌塘地体可能具有古老的结晶基底；中央隆起区上地壳变形主要以逆冲、褶皱为主，下地壳出现北倾与南倾“对冲”的反射，揭示出印度和欧亚两大板块前缘汇聚的深部过程.

Testing deep seismic reflection profiles across the central uplift of the Qiangtang terrane in the Tibetan Plateau

A test of deep seismic reflection profiling across the central uplift or metamorphic belt of the Qiangtang terrane, Tibet Plateau, provides a first image of the crustal structure. There may be old crystalline basements in the Qiangtang terrane; Complex reflection patterns in the upper crust are interpreted as a series of folds and thrusts, and bivergent reflections in the lower crust may represent a convergence between the Indian and the Eurasian plates.