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查证测区内发育晚二叠世敌布错组,将原中侏罗世达雄群修定为二叠纪地层,完善与丰富了二叠纪地层系统。将原“木嘎岗日群”修定为沙木罗组。获得了一批重要的古生物和同位素年龄资料,重新修定了班戈-八宿地层分区与隆格尔-南木林地层分区的界线。新发现晚白垩世中—基性杂岩、始新世造山型环斑花岗岩及新近纪白榴石响岩。新发现阿索构造混杂岩带和具特大型远景的富磁铁矿、具中型远景的铜多金属矿各1处。
The Late Permian Ubu Buluo Formation was verified in the survey area, and the original Middle Jurassic Daixiong Group was rebuilt into Permian strata, which perfected and enriched the Permian stratigraphic system. The original “Mogagangrinshi group” was revised as salamulo group. A number of important palaeontological and isotopic dating data were obtained and the boundaries between the Bangor-Bessu stratigraphic subregion and the Longger-Namu Lam stratigraphic subregion were reworked. Late Cretaceous mid-mafic complex, Eocene orogeny ringed granite and Neogene leucite rock. The newly discovered Asaux tectonic melange belt and rich magnetite with extra-large vistas and one copper-polymetallic ore with a medium-sized prospect are newly discovered.