Bangong Co-Nujiang suture zone, Tibet-a suggestion given by deep geophysical structure
zhao wenjin1; liu kui2; jiang zhongti1; wu zhenhan2; zhao xun1; shi danian3; xiong jiayu1; j.mechie4; l.brown5; t.hearn6; j.r.guo5; seth s. haines7(1. chinese academy of geological sciences; beijing 100037; china; 2. institute of geomechanics; chinese academy ofgeological sciences; beijing 100081; china; 3. institute of mineral resources; chinese academy of geological sciences; beijing 100037; china; 4. geoforschungs zentrum potsdam; potsdam; germany; 5. department of geological sciences; cornell university; ithaca; ny; usa; 6. department of physics; new mexico university; las cruces; nm 88003; usa; 7. department of geophysics; stanford university; stanford; california; usa)
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Ages of volcanic rocks and planation surface in the Canmei Mountain area, northern Tibet
li jindong1; 4; bai daoyuan2; 3; wang xianhui2(1. china university of geosciences; beijing 100083; china; 2. hunan institute of geology survey; xiangtan 411100; hunan; china; 3. faculty of resources; china university of geosciences; wuhan 430074; hubei; china; 4. hunan bureau of geology and mineral exploration and development; changsha 410011; hunan; china)
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