发现了有化石依据的早古生代地层;在果干加年山发现大量的古生物化石;在中浅变质岩解体出早二叠世地层;否定了羌塘中部隆起区存在中元古界变质基底;羌北发现石炭—二叠纪较为连续的类化石序列;发现上泥盆统;厘定了新近系康托组与唢呐湖组的对应关系;在尼玛县绒玛乡温泉附近和古木乡南西采集了大量头足类、笔石、竹节石等化石;补充、厘定完善了羌南、羌北岩石地层序列;石炭纪基性岩墙群和羌塘中部面积最大的复合岩基———本松错岩体以及新近纪火山岩研究取得进展;在角木日地区发现一套保存完整的蛇绿岩;发现和确定了果干加年山构造混杂岩体;进一步探讨了羌塘基底和南北向构造问题。 Discovered fossil-based Early Paleozoic strata, found a large number of paleontological fossils in the stem area and the Giant Mountains, disintegrated the Early Permian strata in the middle-shallow metamorphic rocks, denied the existence of the Mesoproterozoic metamorphic basement in the uplift area of ​​the Qiangtang area, In the northern Qiangtang, the continuous Permian fossil sequences of Carboniferous and Permian were found; the Upper Devonian was found; the corresponding relationship between the Neogene Cantor and the Suonahu Formation was determined; near the hot springs of Rongma Township in Nima County and the southwestern of Gu Muxiang A large number of fossils such as cephalopods, penoliths and slubby stone were collected. Complementary sequences of rock formations in the Qiangnan and Qiangbei areas were determined and perfected. Carboniferous basement dyke groups and the largest composite rock base in the central part of Qiangtang The progress of the study on the Songxian fault pluton and the Neogene volcanic rocks; the discovery of a set of preserved ophiolite in the Kokmuri area; the discovery and determination of the Ganjuganshan tectonic mélange; further exploration of the Qiangtang basement and the north-south To construct the problem.