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在地层、古生物、区域构造、第四纪地质等方面取得若干新进展。如:查明吉隆沟前寒武纪至侏罗纪地层剖面完全可与经典的聂拉木-樟木剖面对比,是喜马拉雅地区又一极为重要的剖面;进一步确定了雅鲁藏布江结合带具有分带特征,并划分出南、北2个不同时期的蛇绿混杂岩带;在扎东、穷果等地发现多处古人类活动遗迹。
In the strata, paleontology, regional tectonics, quaternary geology and made some new progress. For example, it is clear that the profile of the Precambrian-Jurassic stratigraphic zone in JiLilong can be completely compared with the classic Nyalam-Zhangmu profile and is another extremely important section in the Himalayas. It is further confirmed that the Brahmaputra junction belt has zonation characteristics , And divided into two different periods of ophiolitic mélange belt in south and north. Many ancient human activity relics were discovered in Zhaodong and Qiongguo.